Based on a large number of field investigations and laboratory tests, according to the physical parameters of different debris flow deposits on site, the viscosity range of debris flow slurry and the solid particle gradation of debris flow are determined. Through the test, the water and soil ratio of slurry in different viscosity range is determined, and debris flow slurry with different viscosity is configured according to the water and soil ratio. Through the screening test, the solid particle gradation of debris flow is determined. Considering the different combinations of three factors of debris flow slurry viscosity, solid ratio and particle gradation, the debris flow siltation bodies in different states are manually configured, and the bearing capacity test of debris flow siltation bodies is carried out to study the consolidation characteristics and temporal and spatial variation characteristics of bearing capacity of debris flow siltation bodies with different viscosity, solid ratio and particle gradation.
LIU Bin , SU Na , XU Linrong , CHEN Hongkai
(1) Data content: This data set is based on the Xiaguiwa landslide in the Sanjiang basin of the Qinghai-Tibet Plateau, reconstructing the bedding slope of the Xiaguiwa landslide; the bedding slope of the Xiaguiwa landslide is used as a reference for shaking table model tests, which is used to design the shaking table model test model and sensor layout diagram for the bedding rock slope, with a weak rock layer in the model slope, and the sensors deployed are acceleration sensors and velocity sensors, and the measured (2) Data source and processing method: The data set is drawn by Guo Mingzhu of Beijing University of Technology using CAD software. (3) The data provide reference for the subsequent shaking table model test implementation.
GUO Mingzhu
(1) Data content: This data set is based on the Xuelongnang landslide in the Sanjiang basin of the Qinghai-Tibet Plateau, and reconstructs the counter-bedding slope before the slide; the counter-bedding slope before the slide is used as a reference for the shaking table model test, which is used to design the shaking table model test model and the sensor layout diagram for the counter-bedding rock slope, and a special joint is set in the model slope, and the deployed sensors are the acceleration sensors and the velocity sensors. (2) Data source and processing method: The data set is drawn by Guo Mingzhu of Beijing University of Technology using CAD software. (3) The data provide reference for the subsequent shaking table model test implementation.
GUO Mingzhu
This sub topic obtains the physical and mechanical indexes of sliding zone soil and bedrock of typical major landslides (zanong landslide, zongrongcun landslide and xiaguiwa landslide) in Jinsha River Basin of Qinghai Tibet Plateau. The physical and mechanical indexes of sliding zone soil are mainly obtained by large-scale direct shear test. The obtained physical and mechanical indexes provide a scientific basis for subsequent physical model tests and revealing the internal and external dynamic coupling mechanism. The shear strength test of sliding zone soil adopts large-scale direct shear instrument, and there are three groups considering different moisture content. In the large-scale direct shear test, the remolded sliding zone soil specimens with different moisture content are made for three typical landslides respectively, and the shear strength normal pressure relationship curve of sliding zone soil with different moisture content is obtained, and then the shear strength index of sliding zone soil with different moisture content is obtained.
YAO Aijun
This sub topic obtains the physical and mechanical indexes of bedrock of typical major landslides (zanong landslide, zongrongcun landslide and xiaguiwa landslide) in Jinsha River Basin of Qinghai Tibet Plateau. The physical and mechanical indexes of bedrock are mainly obtained through point load test. The obtained physical and mechanical indexes provide a scientific basis for subsequent physical model test and revealing the internal and external dynamic coupling mechanism. The strength test of typical landslide rock block adopts point load instrument, with no less than 15 specimens in each group, a total of 5 groups. There are five kinds of rock samples for point load test, namely limestone, ophiolite, mica gneiss, diorite and schist. Among them, diorite is loaded in cylindrical radial direction, and the rest are irregular rock samples. The size of the experimental results is corrected, and the experimental state is natural water content.
YAO Aijun
We have studied the Petrotectonic attributes of granites distributed in a large area in the North Lancangjiang structure in Bitu area. The major and trace elements and Sr Nd isotopes have been completed in the Key Laboratory of deposit geochemistry, Institute of geochemistry, Chinese Academy of Sciences. Among them, the main elements are analyzed by pw4400 X-ray fluorescence instrument, and the contents of 10 element oxides are determined; Trace elements are tested by ICP-MS inductively coupled plasma mass spectrometer. ICP-MS is manufactured by Agilent company in Tokyo, Japan, and the model is Agilent 7700x. The analysis method is the same as that of Zhang Xin, etc. According to the analysis results of standard sample gbpc-1de, the analysis error is less than 5%. MC-ICP-MS double focusing magnetic mass spectrometer with Neptune plus model is used for isotope test experiment. The test basis is GB / T 17672-1999.
WANG Shifeng
The research on mixing different types of curing agents into debris flow siltation body has great engineering significance. It can not only make up for the deficiency of previous research on the curing characteristics of debris flow siltation body, but also provide a scientific basis for solving the difficulty of debris flow rescue and dredging the main traffic roads in time to a certain extent. In order to study the solidification characteristics of debris flow sediment, Central South University carried out indoor debris flow sediment solidification experiments to study the variation law of bearing capacity of debris flow sediment under the action of different types and different amounts of cement curing agent under the conditions of different gradation and different moisture content, so as to provide reference basis for better handling emergency rescue.
SU Na
The abrasion characteristics of debris flow are the key parameters for the durability design of prevention and control engineering. In this project, 44 working conditions of 5 kinds of gravel gradation, 4 solid ratios, 3 kinds of slurry viscosity of debris flow, 2 kinds of debris flow velocity and 2 kinds of concrete strength are selected. The debris flow abrasion test is carried out with the self-developed debris flow abrasion test device to examine the concrete loss rate Changes of abrasion rate and surface morphology. The experimental results show that the loss rate and abrasion rate of concrete increase with the grading number of gravel (the content of large particle gravel increases), the solid ratio of debris flow and the viscosity of debris flow. According to the developed debris flow abrasion test device, the debris flow abrasion test of concrete materials is carried out, the debris flow abrasion test results are obtained, and the debris flow abrasion coefficients of different concrete materials are obtained
JIAO Pengpeng , SU Na , XU Linrong
Experimental data of impact force of debris flow block stone. The yield stress of impact medium, particle size of impact medium, impact force of block stone and other data produced by the impact force model test of debris flow block stone carried out in the State Key Laboratory of geological disaster prevention and geological environment protection; The data collection place is the State Key Laboratory of geological disaster prevention and geological environment protection of Chengdu University of technology. The data are obtained through the impact force model test of debris flow blocks. The main instruments used include HAAKE rotary rheometer mars40 / 60, HD camera, qsy8301-01 piezoelectric sensor, etc. the collection time is 2019-2021.
LIU Qinghua , SU Na , XU Linrong
The effects of different control factors such as clay content, width height ratio, upstream inflow flow and initial water content on the collapse of gully blocking landslide material source are studied. Through the analysis of the collapse process of weir plug body, the collapse modes of weir plug body are classified. This paper summarizes the longitudinal evolution law of dam body contour under different failure modes, calculates the flow depth, flow velocity and erosion rate, analyzes the temporal and spatial evolution process of dam body under different failure modes, discusses the effects of different factors on the gravity of dam break debris flow and peak discharge, and establishes the mathematical model of dam break discharge amplification coefficient of weir plug dam, Two plugging points in the study area and one plugging point in Ginkgo Pinggou are selected for verification, but there are some limitations in practical application due to the complexity of weir plug dam failure.
ZHANG Youyi
A large number of engineering practices show that the total amount of slope material sources and dynamic reserves account for a large proportion of the total amount of material sources in the basin, which is an important source of debris flow after the earthquake. Through the indoor model test, this paper analyzes the sensitive factors of slope material source rainfall start-up, compares and analyzes the estimation results of slope material source dynamic reserves by engineering experience method and RUSLE model, and reveals the influence of slope re greening herb vegetation on slope material source seepage field through numerical simulation analysis on the basis of indoor model test.
ZHANG Youyi
Aiming at the material source of "wide, gentle" and "narrow and steep" debris flow gully, based on field investigation and indoor rock and soil mechanical parameter test, this study uses indoor model experiment to study the starting mechanism of loose material in gully under different influencing factors. Through data analysis and fitting, the dynamic reserve model of gully provenance is established, which provides reference and scientific basis for the prediction, early warning and treatment engineering design of similar debris flow gully in earthquake area. The main conclusions are as follows: (1) The incipient erosion processes of deposits with different structural types are different: fine-grained soil appears rills at the front edge after the start of runoff at the rear, and gradually develops into pull grooves, which run through to the rear edge; After the runoff of coarse-grained soil starts, the front edge collapses and slides, showing the characteristics of traceability erosion; The upper fine and lower coarse soil first formed grooves at the boundary of soil layer and gradually extended to the rear edge; The upper coarse and lower fine soil first form a rill at the front edge, and the coarse soil in the back layer slides and scrapes the fine soil at the front edge. (2) At the moment of debris flow starting, coarse particles are mainly started in the form of sliding, jumping and rolling, and the starting and migration forms of coarse particles in fine-grained soil are mainly rolling and jumping; In coarse-grained soil, the coarse particles are mainly started by sliding; The confluence of upper fine and lower coarse soil is dominated by rolling and jumping in the early stage, and sliding in the later stage; The coarse particles in the upper coarse and lower fine soil start mainly by sliding. (3) The greater the rainfall intensity, the greater the runoff, and the stronger the undercutting erosion. The erosion curve tends to increase first and then decrease, and the maximum erosion depth generally appears at the place where the slope changes steeply and gently. (4) Based on the indoor simulation test results and fractal dimension theory, the evaluation model of "wide and slow" channel source dynamic reserves is established and verified.
ZHANG Youyi
The researchers of the research group carried out field investigation on the typical "wide and gentle" gully debris flow gully - Wenchuan Qipan gully and "narrow and steep" gully debris flow gully - Beichuan Qinglin gully branch. Through the field particle screening test of typical channel deposits in qipangou, and the qualitative and quantitative description of channel shape and typical channel section, it is found that the wide and gentle channel material source has the characteristics of "wide gradation, weak consolidation and easy stratification"; In addition, the debris flow accumulation samples of Qinglin gully branch gully are selected for on-site particle screening test, and the clay content, porosity and shear strength of the test soil samples are determined.
ZHANG Youyi
The photos include daily (2021.7.25-2021.8.6) scientific research disaster points and working photos, as well as the questionnaire of each disaster point (including landslide, collapse, debris flow, etc.), identify the disaster points recorded every day on the map, convert them into KMZ format, and analyze the distribution of disaster points in the scientific research area on GIS. The distribution of disaster points shows that there are fewer disaster points along the north line and in the scientific research county, while there are more disaster points along the south line and in the scientific research county. During the scientific research, wind sand points and mountain erosion points were found and recorded. Especially in the valleys and gullies around the Himalayas, disasters such as landslide and debris flow are easy to occur, while geological disasters are not easy to occur in the Qiangtang plateau area (plateau surface). The photos of disaster points can reflect the disaster characteristics of a region. They are intuitive data for studying local disaster types, and then have basic significance for local disaster types, distribution and disaster prevention and reduction measures.
ZHOU Qiang, NIU Baicheng , HUAQUE Cairang , LI Chunhua , ZHANG Shengpeng , MA Mingfu , GAO Haixin , CHEN Yingming , DING Yuanhui , GAO Yuan
The period of real-time monitoring of landslide data from 2020.6 to 2022.7, and the original monitoring data of Newton's geological disaster monitoring center is 2022-2020. Through the Newtonian force monitoring of 6 points, the real-time change of deep Newtonian force can be obtained in time, and the data can be fed back to the experimental analysis center synchronously. The analysis center draws the Newtonian force change curve synchronously, and the system can intelligently determine whether there is a landslide disaster in the measuring point area based on the landslide Newtonian force early warning criterion, In case of the sudden drop of Newtonian force, timely feed back to the local management department according to the change degree of sudden drop. This data can be used as a criterion for the occurrence of landslide, and the system can provide scientific guidance for the prevention and control of active fault landslide disasters.
TAO Zhigang
1) Data content: this data set is the landslide disaster data of Sanjiang Basin in the southeast of Qinghai Tibet Plateau; 2) Data source and processing method: this data set was independently interpreted by Dai Fuchu of Beijing University of technology using Google Earth; This data file is finally formed by remote sensing interpretation - on-site verification - re interpretation - re verification and other methods after 7 systematic interpretation. More than 5000 landslides have been verified on site with high accuracy; 4) This data has broad application prospects for hydropower resources development, traffic engineering construction and geological disaster evaluation in the three river basins in the southeast of Qinghai Tibet Plateau.
DAI Fuchu
The process of reconstructing the river blocking disaster chain in Yajiang river basin is of great significance to deeply understand the natural attributes and evolution law of ice river lake water landscape system in natural state. This data is the digital surface elevation model obtained in the process of scientific research. The data source is UAV tilt photography, which is corrected by real-time differential GPS (RTK) control points; The vertical resolution is 5cm and the horizontal resolution is 20cm. This data can be used to assist in identifying the spatial distribution of break flood sediments (break flood hills, gravel hills, Boulder core beach, etc.) in typical manqu river reach and the position of weir plug dam body, so as to obtain the section elevation. It is the first-hand data for restoring the scale of break flood.
ZHAO Zhijun , CAO Xilin
This data is the disturbance disaster data of 1:250000 major projects in the Qinghai Tibet Plateau. For the scope of disaster interpretation, line engineering (national highway, high-speed, railway and Power Grid Engineering) and hydropower engineering are bounded by the first watershed on both sides of the project; Mine, oilfield and port projects are bounded by 1km away from the project. Engineering disturbance disasters can be divided into two categories: ① landslide, collapse and debris flow disasters induced by engineering construction; ② For natural disasters that may affect the project, it is stipulated that all natural disasters within the above interpretation scope belong to category ② engineering disturbance disasters. The data includes the location, length, width, height difference, distribution elevation, genetic type, inducing factors, occurrence time, lithology and other elements of landslide, disaster related projects and project construction years. Based on Google Earth image and 1:500000 geological diagram, 6176 disaster points were interpreted; Google Earth is mainly used for disturbance disaster interpretation, and combined with field investigation to verify the interpretation results, ArcGIS is used to generate disaster distribution map; The data comes from Google Earth high-resolution images, with high accuracy of original data. In the process of generating disaster files, the interpretation specifications are strictly followed, and special personnel are assigned to review, so the data quality is reliable; Based on the collected data, the disaster risk analysis of the study area can be carried out to provide theoretical guidance for the smooth operation of the built projects and the construction of the line projects not built / under construction.
QI Shengwen
Dating data of debris flow and dammed lake sediments in complex mountainous areas from 2019 to 2021. The data collection sites are complex mountainous areas prone to debris flow in the eastern and southern edges of the Qinghai Tibet Plateau. The experimental analysis is mainly completed in the salt lake chemical analysis and testing center of Qinghai Salt Lake Research Institute of Chinese Academy of Sciences and the analysis and testing center of Chengdu Mountain Institute of Chinese Academy of Sciences. The instruments used include RIS ø TL / OSL – Da – 20 automatic luminescence instrument, etc. The age data set of debris flow sediments in typical complex mountainous areas is established, the formation age of debris flow sediments in complex mountainous areas is quantitatively studied, and the ancient debris flow disaster activity history in complex mountainous areas is determined.
HU Guisheng
The single mineral EPMA data set of magmatic rocks in the Himalayan orogenic belt is mainly based on the main data of single minerals in Jilong area, and the test points of single minerals are more than 200. The rock is light colored granite. The single minerals tested are mainly feldspar, garnet, muscovite and biotite. The single mineral electron probe uses cameca sxvivefe electron microprobe, etc. The data has not been published, and the data results are true and reliable. The testing units are mainly the Institute of geology, Chinese Academy of Geological Sciences and the Institute of mineral resources, Chinese Academy of Geological Sciences. The data set can be used to study the petrogenesis of leucogranite melts in the Himalayan orogenic belt.
ZENG Lingsen , GAO Lie , YAN Lilong
1) This paper describes a new species of Sinoalidae from the Daohugou biota of Middle to Late Jurassic, revises the synonym jiania, and proves the correlation between the Daohugou fossil bed and the Jiulongshan Formation in Luanping. 2) The fossil materials come from Daohugou area, Ningcheng County, Chifeng City, Mongolia in the Middle to Late Jurassic of China. The images of the fossils are imaged by V16 stereomicroscope, the plates are made by PS software, and the line drawings are drawn by CDR software. 3) The new species is based on two fossils, which are preserved in tuff shale. 4) This paper proves the stratigraphic correlation between Daohugou bed and Jiulongshan Formation in Luanping, Hebei Province from the perspective of biostratigraphy.
FU Yanzhe
This data belongs to U-Pb geochronology data of Hailaer Basin in eastern China, including Pb, 232Th, 238U contents, 207Pb / 206Pb, 207Pb / 235U, 206Pb / 238U ratios and errors, 207Pb / 235U, 206Pb / 238U ages and errors, etc. The data belongs to LA-ICP-MS data, and the precision and accuracy meet the research requirements. The results of geochronology data play an important role in the establishment of Mesozoic stratigraphic framework in Hailaer basin, which lays a good foundation for the Mesozoic tectonic evolution and basin analysis in this area, and has a good application prospect.
ZHU Jichang
This data belongs to U-Pb geochronology data of Mesozoic strata in Huanghua depression, Bohai Bay Basin, inner North China Craton, including Pb, 232Th, 238U contents, 207Pb / 206Pb, 207Pb / 235U, 206Pb / 238U ratios and errors, 207Pb / 235U, 206Pb / 238U ages and errors, etc. Zircon U-Pb dating was carried out by using the second upgraded excimer laser ablation system (geolas HD, 193nm wavelength) and laser ablation inductively coupled plasma mass spectrometry (ICP-MS) with quadrupole (Agilent 7900). The laser frequency is 5Hz and the beam size is 30 nm μ m。 The international standard sample 91500 was used as the external calibration standard for age calculation. Nist610 was used to calculate the concentrations of uranium, thorium and lead, and gj-1 was used to monitor the isotopic ratios The U-Pb isotopic ratios were calculated by cal10.8, and the common Pb was corrected by compb # 3-18. The age of particles younger than 1000mA is based on their 206Pb / 208U ratio. The analysis with > 10% or < – 5% inconsistencies was excluded. The acceptable inconsistencies and accuracies of the analysis were listed in the table below. The harmonic age and the mean age were calculated by isoplot software. The uncertainty of the mean age was 2 σ, The individual analysis report is 1 σ。 The results of geochronology data are published in Science China earth science, and the data quality is reliable. It plays a very important role in the establishment of Mesozoic stratigraphic framework in Bohai Bay Basin covered by Cenozoic. It lays a good foundation for Mesozoic tectonic evolution and basin analysis in this area, and has a good application prospect.
ZHU Jichang
This map is the result of the project of deep process and resource effect of Yanshanian major geological events, and it is the "Temporal and spatial distribution map of Yanshanian tectonic-magmatic-deposits in Northeast Asia". The diagram systematically summarizes the temporal and spatial distribution of magmatic rocks and deposits in the Yanshanian tectonic period (Jurassic and Cretaceous) in Northeast Asia. The geochronological data, the distribution of magmatic rocks and ore deposits in the map are derived from the papers published during the implementation of the project and previous studies on the geological period. The map can reveal the internal relationship among Yanshanian tectonism, large-scale magmatism and metal mineralization in Northeast Asia, and point out the exploration direction of dominant metal minerals in typical areas.
ZHANG Lipeng
This data set mainly includes the results of Zn isotope and trace element analysis of iron rich peridotites and pyroxenites from the central European Bohemian orogenic belt. The samples are from the late Paleozoic. The samples include mg rich peridotite, Fe rich peridotite and pyroxenite. The Zn isotopic data were obtained by MC-ICPMS after acid digestion and ion exchange resin separation, and the trace element data were obtained by ICP-MS after acid digestion. After acid digestion, the trace elements were determined by ICP-MS, separated by ion exchange resin, and then determined by MC-ICPMS.
In this data set, the modern standard sample srm683 developed by the National Institute of standards and technology of the United States is used for Zn isotope analysis. The Zn block obtained at the University of science and technology of China is located at 31 N latitude ° 5 ', 117 e °。 Zn isotope data were obtained by MC-ICPMS after acid digestion and ion exchange resin separation. After the sample was digested by acid and separated by ion exchange resin, MC-ICPMS was used to test the zinc isotope, and international standard samples were selected to monitor the test data. The obtained Zn isotopic data can be used as a new international interpolation standard for the establishment of ZB isotopic analysis method by international peers in the future, and provide important significance for the comparison of data between laboratories
HUANG Fang
This data set mainly includes Zn isotopic analysis of island arc magmatic rocks obtained from Kamchatka islands and Aleutian Islands. The locations include eastern Kamchatka, central Kamchatka, Atka and umanka islands. The Zn isotopic data were obtained by MC-ICPMS after acid digestion and ion exchange resin separation of whole rock samples. The whole rock sample was crushed to less than 200 mesh without pollution, and the powder was digested by acid and separated by ion exchange resin. Then the zinc isotope was tested by MC-ICPMS. The international standard samples were selected to monitor the test data. The obtained data of island arc magmatic rocks provide important information for Zn isotopic reservoir composition of oceanic basalts.
This data set mainly includes Cu isotopic analysis of orogenic peridotites from the everea Alps, Italy, in balmucha and baltisa. Zn isotopic data were obtained by MC-ICPMS after acid digestion and ion exchange resin separation. The whole rock sample was crushed to less than 200 mesh without pollution, and the powder was digested by acid and separated by ion exchange resin. Then the zinc isotope was tested by MC-ICPMS. The international standard samples were selected to monitor the test data. These peridotite Zn isotopic data provide important information for mantle reservoir Zn isotopic composition.
This data set mainly includes Cu isotopic analysis of orogenic peridotites from the everea Alps, Italy, in balmucha and baltisa. Cu isotopic data were obtained by MC-ICPMS after acid digestion and ion exchange resin separation of whole rock samples. The whole rock sample was crushed to less than 200 mesh without pollution, and the powder was digested by acid and separated by ion exchange resin. Then the copper isotope was tested by MC-ICPMS. The international standard samples were selected to monitor the test data. The data quality has reached the international first-class level. The results provide important information for the Cu isotopic composition of peridotite reservoirs.
This data set mainly includes the results of Cu and Zn isotopic analysis of mid ocean ridge basalts obtained from iodp1256 borehole in the Pacific Ocean. The sample types include volcanic rocks, sheet dikes, transition zones and gabbros. The Cu and Zn isotopic data were obtained by MC-ICPMS after acid digestion and ion exchange resin separation of whole rock samples. The whole rock sample is crushed to less than 200 mesh without pollution, and the powder is digested by acid and separated by ion exchange resin. Then, the copper and zinc isotopes are tested by MC-ICPMS. The international standard samples are selected to monitor the test data, and the data quality reaches the international first class.
This data is the data of major, trace and rare earth elements, zircon U-Pb age and pyroxene geochemistry of basalt rhyolite whole rock of massive sulfide deposit in hamamid area, Eastern desert of Egypt. The major element data of the whole rock were obtained by XRF analysis, the trace and rare earth element data were obtained by ICP-MS analysis, the zircon U-Pb dating data were obtained by LA-ICP-MS analysis, and the major element composition of pyroxene was obtained by electron microprobe analysis. The above data have been published in high-level SCI journals, and the data are true and reliable. Through the data obtained, the magmatic evolution process can be described, so as to better restrict their relationship with sulfide deposit mineralization.
YANG Xiaoyong
This data set is derived from the paper: Ma, L. *, Wang, Q. *, Kerr, A.C., Yang, J.H., Xia, x.p., ou, Q., Yang, Z.Y., sun, P., 2017. Paleocene (ca. 62 MA) leucogenes in southern Lhasa, Tibet: products of syn colonial strategic analysis during slab roll back? Journal of petroleum, 58 (11): 2089-2114. This research achievement is supported by the special project "deep process and resource effect of major geological events in Yanshanian period" (2016yfc0600400) of national key R & D Program "exploration and exploitation of deep resources". This achievement is a part of the research achievements of associate researcher Ma Lin, researcher Wang Qiang and their team in petrology and deep dynamics of the Qinghai Tibet Plateau. The team applied petrological and geochemical methods to reconstruct the collision evolution history of the southern margin of the Himalayan Tibetan Plateau orogenic belt. The Paleocene (63-58 MA) garnet two mica granite and biotite granite assemblage were determined by the applicant in Gangdise. It is found that the two types of rocks have the same sr-nd-hf-o isotopic composition, but the major elements show the characteristics of increasing with the increase of Si Al composition and decreasing with the decrease of Mg Fe composition. At the same time, similar mineral composition evolution is found, including the transformation from mg biotite to iron biotite, the continuous composition evolution of medium feldspar Pei feldspar aofeldspar albite, and the increasing composition of garnet core to edge, It is revealed that garnet two mica granite is the product of high differentiation evolution of Cenozoic lower crust melt, which provides petrological evidence for the high differentiation genesis of I-type leucogranite. The study also reveals that the Gangdise syn collisional anatexis is related to the diachronic collision of the Indo subcontinent. The interaction model of continental collision and oceanic subduction also provides reference and Enlightenment for understanding the abnormal thermal phenomena of the crust and lithosphere in the global large convergent orogenic belts. The data are from the appendix of this paper. The data set includes: 1. Data of major oxides and trace elements; 2. Whole rock SR Nd isotopic data; 3. Sims zircon U-Pb dating data; 4. LA-ICP-MS zircon U-Pb dating data; 5 zircon HF-O isotope data.
MA Lin
The data is in JPG format. Through the experimental data, zircon chronology and trace element analysis data, the whole rock geochemical analysis data. Zircon geochronology data were analyzed by LA-ICP-MS in mass spectrometry Laboratory of School of resources and environmental engineering, Hefei University of technology. The whole rock geochemical analysis was carried out in the EPMA laboratory, School of resource and environmental engineering, Hefei University of technology. The instrument used was jeol-jxa-8230 EPMA analyzer of Japan Electronics Company. The results of JPG data include: geological map of Dabie orogenic belt, geological sketch of Dabie structure, static photos of migmatite samples, cathodoluminescence map of zircon in gneiss and dark enclave, concordance map of zircon, classification map of feldspar, composition map of calcareous amphibole, classification map of biotite, and mafic map of biotite. This data can provide evidence support for genetic analysis of migmatite in North Dabie.
YAN Jun
Data includes excel and JPG format. Excel data includes: whole rock major and trace element analysis data, whole rock strontium and neodymium isotope analysis data, whole rock Pb isotope analysis data. . In Guizhou Tongwei Analytical Technology Co., Ltd. (Guiyang, China), the whole rock macro and trace elements were analyzed by using Axios pw4400 X-ray fluorescence spectrometer and thermal X Series 2. Strontium and neodymium isotopes were analyzed by MC-ICP-MS at the University of Queensland. This data can provide evidence for the genesis of alkaline A-type granites and the geodynamic background of Early Cretaceous in southeastern China. Data in JPG format include: 1. Distribution of Mesozoic granitoids and volcanic rocks in South China 2. Simplified geological map of Mucheng pluton. 3. Microscopic specimens of granodiorite in Mucheng area. 4. Cathodoluminescence (CL) images of zircon crystals selected from typical Mucheng quartz monzonite and granite 5. Zircon U-Pb concordance of representative quartz monzonite and granite 6. Histogram of zircon HF values in representative rocks 7. Chemical classification of rocks in Muchen rock 9. Chondrite normalized REE 10.87sr/86sr and ε Nd (T) diagram of muchenyan. 11. Whole rock lead isotope analysis 12. Zircon saturation temperature and Ti histogram of Mucheng quartz monzonite 13. SiO2 and Ti and SiO2 and Zr of Mucheng quartz monzonite 15. Rb / Sr and BA / RB, Zr / HF and Nb / Ta, th / Yb and BA / La 16. Nd and Hf isotopic map of Mucheng pluton. 17. SiO2 and Mg diagram of Mucheng quartz monzonite and simulated magma
WANG Fangyue
Data includes excel and JPG format. Excel data includes: Zircon chronology data, whole rock major and trace element analysis data, whole rock strontium and neodymium isotope analysis data, zircon hafnium isotope analysis data. Laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) was used for zircon dating in the school of resources and environmental engineering, Hefei University of technology, China. The major and trace elements of the whole rock were measured in ALS laboratory group (Australian ICP-MS analysis laboratory in Guangzhou, China). The main elements were determined by X-ray fluorescence spectrometry (XRF). Determination of trace elements by ICP-MS on element-2 mass spectrometer RB – Sr and SM – Nd isotope measurements were carried out on the Finnigan mat ‐ 262 thermal ionization mass spectrometer (TIMS) of University of science and technology of China. The State Key Laboratory of geological processes and mineral resources of China University of Geosciences has carried out in-situ Hf isotope analysis on zircon grains, which have been dated by la-icp-ms. The data in JPG format include: (1) geological map of Dabie orogenic belt showing the distribution of Early Cretaceous rocks; (2) geological map of sigongshan area in central Dabie; (3) microscopic image of magmatic rocks of sks intrusion (cross polarized light) (a) quartz diorite (14sk003-1); (4) quartz diorite (14sk003-1); (4) quartz diorite (14sk003-1); (4) quartz diorite (14sk003-1); Four representative zircon cathodoluminescence (CL) images of sks intrusions 5. Zircon u – Pb concordance of sks intrusions 6. Classification of sks intrusions; Harker diagram of sks intrusive magmatic rocks 9. Rb-v of magmatic rocks of sks intrusion. 10 SR – Nd isotopic composition of sks intrusion data source: 11 zircon U-Pb age and age. ε HF (T) diagram of sks intrusive magmatic rocks: 12 (LA / Yb) n-sr / y diagram of sks intrusive magmatic rocks; 13 EU and Sr (a) and EU and Rb (b) diagram of quartz diorite and monzonitic granite in sks intrusion; 14 y and Sr / y fractional crystallization (FC) model Based on the above data, we can analyze the monzogranite and quartz diorite in sigongshan pluton, the largest pluton in the central Dabie unit of Dabie orogenic belt, and provide evidence for their movement analysis in Mesozoic geodynamics.
YAN Jun
This data set comes from the following papers: 1. Bai, Z. - J., Zhong, H., Hu, R. - Z., Zhu, W. - g., 2020. Early sulfur saturation in arc volcanic rocks of southern China: implications for the formation of CO massive porphyry – epichermal Cu – Au deposits. Geochemica et cosmochemical Acta, 280:66-84. The major and trace data, PGE and Au contents of the whole rock limit the crystallization differentiation process and sulfide saturation history of the magma. Furthermore, the contribution of sulfide re dissolution to the mineralization of porphyry shallow geothermal Cu Au deposits is revealed. The data is from the paper table. 2. Feng, Z. - Z., Bai, Z. - J., Zhong, H., Zhu, W. - g., Zheng, S. - J., 2020. Genesis of volcanic rocks in the Zijinshan ore district, SE China: implications for porphyry epithermal mineralization. Minerals, 10 (2): 200, Zircon HF-O isotope limits the source characteristics, magmatic properties and differentiation evolution process of volcanic rocks, and further reveals the metallogenic potential of magmatism in this period.
BAI Zhongjie
There are two kinds of data: Excel table and JPG model analysis chart. The Excel data show that the major and trace elements of the whole rock were measured in the ALS laboratory group (Australian ICP-MS analysis laboratory in Guangzhou, China). The main elements were determined by X-ray fluorescence spectrometry (XRF). Trace elements and rare earth elements were determined by element-2 mass spectrometer. The concentrations and isotopic ratios of Rb – Sr, SM – nd and u – th were determined by isotope dilution method. Zircon geochronology and Hf isotope data are also included. The analysis data of JPG model include: 1. Geological map of Dabie orogenic belt showing early Cretaceous distribution; 2. Geological map of BHY shapinggou molybdenum deposit. 3. The geological section is magmatic rock and ore body of shapinggou molybdenum deposit. 4. According to the data of 313 geological team and Mineral Exploration Bureau of Anhui Provincial Bureau of geology, the sample position and the column section of the borehole are modified. 5. Geological map of Xianghongdian area. 6. Geological map of gongdongchong lead-zinc deposit (a) and A-B section of gongdongchong lead-zinc deposit 7. Zircon cathodoluminescence (CL) images of zircons from shapinggou granite porphyry and gongdongchong quartz monzonite porphyry. White and yellow circles represent the location of U-Pb dating and in site Hf isotope, respectively. The adjacent numbers are the analysis results. 8. Zircon U-Pb concordance map of shapinggou granite porphyry and gongdongchong quartz monzonite porphyry. 9. Chemical composition diagram of BHY ore bearing rocks. 10. (a) chondrite normalized REE patterns and (b) n-morb normalized multi-element spider diagram 11. Initial SR – Nd isotopic composition of ore bearing magmatic rocks in the BHY belt. 12. The initial lead isotopic composition of BHY ore bearing rocks. Ore bearing magmatic rocks include SPG, TJP, DG and QEC 13. Zircon U-Pb age (T) of BHY ore bearing rocks ε Hf（t）。 SiO2 and SiO2 ε Nd (T) nd (T) map of magmatic rocks in Dongchong mining area. 15. Production pattern of Mo Pb Zn granitic rocks in North Huaiyang area. The database data can be used to study the mineralization and relationship of granite porphyry to molybdenite in shapinggou area.
YAN Jun
The data is divided into excel table data and JPG analysis chart data. The table data include: Table 1 the characteristics of grouper samples in southern Anhui Province; Table 2 EPMA data of apatite in granodiorite from southern Anhui Province; Table 3 LA-ICP-MS data of apatite in granodiorite from southern Anhui The apatite studied in this study was separated from SAP granodiorite samples by heavy liquid method, and then selected by hand under binocular microscope. The selected apatite was mounted in epoxy resin, polished, and then examined by backscattered electron (BSE) image to select self shaped targets for electron probe microanalysis and laicp-ms analysis. The main elements of apatite were determined by jeol-jxa-8230m electron microprobe at the school of resources and environmental engineering, Hefei University of technology. The trace elements were determined by LA-ICP-MS at the Key Laboratory of Mineralogy and mineralization, Guangzhou Institute of geochemistry, Chinese Academy of Sciences. The analysis data include: (1) micrographs of granodiorite samples from southern Anhui Province, showing mineral composition（ a) LQ, (b) JD, (c) QY, and (d) PL granodiorites. Where: PL = plagioclase; KF = potash feldspar; QZ = quartz; Bi = biotite; HBL = amphibole; AP = apatite; ZrN = zircon (2) backscattered electron (BSE) image of euhedral apatite in granodiorite in southern Anhui Province (3) f (wt%) and Cl (wt%) correlation map of apatite samples in granodiorite in southern Anhui Province (4) normalized REE model of (a) apatite (solid symbol) and host rock (hollow symbol) chondrite and (b) apatite primitive mantle marker in granodiorite in southern Anhui Province (5) geochemical map of apatite samples of granodiorite in southern Anhui Province, showing the characteristics of rock classification and magma source area. (6) trace element discrimination map of apatite (solid symbol) and host rock (hollow symbol) in granodiorite in southern Anhui Province, distinguishing adakite from non adakite (7) Apatite in granodiorite from southern Anhui Province (a) δ CE and δ The changes of oxygen fugacity and temperature were reflected by EU value and (b) logfio2 and t diagram. Among them, MH: magnetite hematite buffer, FMQ: forsterite magnetite quartz buffer, IW: iron pyrite buffer (8) geochemical characteristics of apatite samples from granodiorite in southern Anhui Province to distinguish mineralization and non mineralization This database can be used to explore the relationship between polymetallic mineralization of Mesozoic magma and granodiorite in southern Anhui Province, and to judge the types of unmeneralized rocks and deposits by apatite.
XIE Jiancheng
The data are in the form of pictures, including: (1) micrographs of quartz monzodiorite in Anqing area, showing mineral composition. Among them, pl. plagioclase, KFS. Potash feldspar, HBL. Amphibole, Bi. Biotite, QTZ. Quartz (2) Typical cathodoluminescence photos and U-Pb concordance maps of zircons from Yueshan pluton in Anqing. In the cathodoluminescence image, the small solid line circle represents the LA-ICPMS analysis point, and the large dotted line circle represents the la-mc-icpms Hf isotope analysis point. The formation age of the Yueshan pluton is 138.2 ± 1.7 Ma (3) The geochemical diagrams of zircons from adakitic rocks in Anqing are used to explain the REE distribution characteristics of zircons, to distinguish the classification of zircons, the correlation between Zi HF and Ti in zircon temperature (4) Classification map of petrochemical composition of adakitic rocks in Anqing. The adakitic rocks in Anqing are quartz monzodiorite, which are of paraaluminous high-k calc alkaline series (5) The HAAKE diagram of adakitic rocks in Anqing is used to study the correlation between major and trace elements (6) Chondrite normalized REE partition diagram and n-morb normalized trace element spider diagram of Anqing adakitic rock samples (7) The nd Sr isotopic composition of the adakitic rocks in Anqing falls in the range of Nd Sr isotopic composition of the adakitic rocks in the middle and lower reaches of the Yangtze River metallogenic belt, with mixed characteristics (8) The adakitic rocks in Anqing have high radioactive lead isotopic compositions, which are consistent with those of MORB and early Cretaceous basic rocks in the middle and lower reaches of the Yangtze River (9) Zircon of Anqing intrusion ε HF (T) value and U-Pb age map (10) The diagrams of (a) Sr / Y and y, (b) Sr / Y and (LA / Yb) n, (c) K2O / Na2O and Al2O3 show that the adakitic rocks in Anqing were formed by partial melting of subducted oceanic crust (11) The adakitic rocks in Anqing are (a) La / Yb and La, (b) V and Rb, (c) (87Sr / 86Sr) I and 1 / Sr（ × 104)， (d) ε Nd (T) and 1 / Nd（ × 103), showing partial melting and magma mixing (12) The (a) BA and Nb / y diagrams and (b) Rb / Y and Nb / y diagrams of Anqing adakitic rocks show obvious subduction marks (13) Zircon lgfio2 and t of adakitic rocks in Anqing（ º C) Fig. The adakitic rocks in Anqing have high oxygen fugacity and high temperature. Among them, MH: magnetite hematite buffer, FMQ: forsterite magnet quartz buffer, IW: iron pyrite buffer (14) Genetic model of Anqing Copper Gold adakitic rocks. The Anqing adakites are mainly derived from partial melting of subducted oceanic crust, addition of mantle derived magma and assimilation of Neoproterozoic crustal materials during emplacement.
XIE Jiancheng
The database includes: Table 1 LA-ICP-MS zircon analysis data of adakitic rocks in Anqing area; Table 2 in situ trace element data of zircons from Anqing adakitic rocks; Table 3 major and trace element compositions of adakitic rocks in Anqing area; Table 4 nd, Sr and Pb isotopic compositions of adakites in Anqing area; Table 5 la-mc-icp-ms zircon Hf isotopic compositions of adakitic rocks in Anqing area. U-Pb dating and trace elements were analyzed by LA-ICP-MS in the College of resources and environmental engineering, Hefei University of technology. The analysis of major and trace elements was carried out in Guangzhou ALS laboratory group (a commercial ICP-MS analysis laboratory) by ICP-MS. RB, Sr, SM and Nd isotopic data were measured by MAT-262 mass spectrometer in the laboratory of chemical geodynamics, University of science and technology of China. Through the above data, we can explore the influence of adakite on diagenesis and mineralization, and explain the process of mineralization in Anqing area.
XIE Jiancheng
The data are in the form of jpg images, including: (1) binary curves of (a) Fe and s, (b) Cu and Fe in pyrite samples from baoshantao and Fenghuangshan skarn Cu (AU) deposits (2) Trace element contents of pyrite samples from baoshantao and Fenghuangshan skarn Cu (AU) deposits (3) trace element contents of chalcopyrite from Fenghuangshan skarn Cu (AU) deposits (4) trace element contents of pyrite and brass samples from different stages of baoshantao and Fenghuangshan skarn Cu (AU) deposits (a) Au, (b) AG (c) The relationship between the contents of Pb and (d) sb and as (5) the contents of (a) Pb and Bi, (b) Pb / CO and Ag / Co, (c) Au and Cu in pyrite and chalcopyrite samples from baoshantao and Fenghuangshan skarn copper (gold) deposits (d) (6) LA-ICP-MS trace element correlation of Se Sn and CO as in chalcopyrite from Fenghuangshan deposit. (7) LA-ICP-MS trace element correlation of (a) Co and Ni, (b) se and as, (c) Au and Ni in pyrite and chalcopyrite from baoshantao and Fenghuangshan deposits This data chart provides intuitive results for the study of sulfide mineral characteristics of skarn copper (gold) deposit in Fenghuangshan ore field, Tongling. The article has been published in SCI journals, and the data is true and reliable.
XIE Jiancheng
The data include: (1) (a) tectonic map of China（ b) Geological map of Tongling metallogenic area in eastern China (2) The geological map of Fenghuangshan ore field shows the xinwuli granite intrusion and related copper (gold) deposits (3) Section from tieshantou to baoshantou in Fenghuangshan ore field (4) The geological section of baoshandao skarn type copper (gold) deposit shows skarn mineralization in the contact zone between quartz monzodiorite and lower Triassic carbonate rocks. Abbreviation: GRT: garnet; Di: Diopside; Py: pyrite; CCP: chalcopyrite; Cal: Calcite (5) The mineral micrographs of skarn, ore and granodiorite in Fenghuangshan skarn deposit（ a) Garnet skarn（ b) And (c) medium coarse pyrite and vein chalcopyrite coexist with quartz, and heterohedral magnetite particles in quartz sulfide stage are filled with quartz or chalcopyrite（ d) Xinwuli granodiorite. Abbreviation: GRT: garnet; CHL: chlorite; Mga: magnetite; Py: pyrite; CCP: chalcopyrite; QZ: quartz; KFS: potash feldspar; HBL: amphibole; Bi: biotite
XIE Jiancheng
The data contents include: Table 4 electron microprobe data of pyrite and chalcopyrite in baoshandao and Fenghuangshan deposits; Table 5 LA-ICP-MS trace element data of pyrite in baoshandao and Fenghuangshan deposits; Table 6 LA-ICP-MS trace element data of chalcopyrite in Fenghuangshan deposit; The element composition of pyrite and chalcopyrite was measured by jeol-jxa-8230m electron probe of School of resources and environmental engineering, Hefei University of technology. A total of 50 analysis points were analyzed. The analysis conditions were as follows: accelerating voltage 15kV, probe current 20na, peak diameter 5nm μ m。 The trace element compositions of pyrite and chalcopyrite single crystals were determined by resonance 193nm ArF excimer laser and Agilent 7500a ICP-MS in the State Key Laboratory of isotope geochemistry, Guangzhou Institute of geochemistry, Chinese Academy of Sciences. A total of 150 spots were analyzed. The above data have been published in SCI high-level journals, and the data are true and reliable. The data is stored in Excel.
XIE Jiancheng
The data contents are stored in three excel tables: Table 1: characteristics of typical skarn Cu Au polymetallic deposits in Tongling area; table 2: characteristics of representative Cu (AU) deposits in Fenghuangshan orefield; Table 3 main characteristics, pyrite and chalcopyrite types, pyrite and chalcopyrite structure of Fenghuangshan and baoshandao deposits in each metallogenic stage. Table 1 summarizes the previous research results of typical skarn Cu Au polymetallic deposits in Tongling area. The characteristics of representative copper (gold) deposits in Fenghuangshan ore field are summarized in Table 2. The skarn deposits in Fenghuangshan area are mainly small and medium-sized deposits with copper reserves of about 600000 tons. The skarn stage is mainly composed of garnet, diopside and a small amount of wollastonite, actinolite, chlorite, epidote, magnetite, pyrite and chalcopyrite. The three tables summarize the previous studies and provide a basis for the future study of skarn deposits in Tongling and Fenghuangshan areas. The above data have been published in SCI high-level journals, and the data are true and reliable. The data is stored in Excel.
XIE Jiancheng
The data include: (1) zircon U-Pb concordance, weighted average age and cathodoluminescence (CL) images of representative zircon grains from four intrusions in Chizhou area. The small solid circles in CL images represent the spots of la-mc-icp-ms Hf isotope analysis; The big dot circle represents the spots of laicp-ms analysis. (2) Geochemical map of apatite samples from Chizhou granodiorite (porphyry)（ a) CL and f diagram（ b) Chondrite normalized REE map（ c) Y and Sr diagram（ d) Rare earth element triangle. Note: m, mantle; M-C, mantle crust; C. Crust (3) Classification map of petrochemical composition of Chizhou granodiorite (porphyry)（ a) Total alkali and silica (TAS) diagram（ b) Comparison of a / NK and a / CNK（ c) A.R. - SiO2 diagram, A.R. = (Al2O3 + CaO + Na2O + K2O) / (Al2O3 + Cao – Na2O – K2O). The solid line shows the division among calc alkaline, alkaline and peralkaline（ d) Comparison of K2O and SiO2 (4) (a) the relationship between Al2O3 and SiO2 of Chizhou granodiorite (porphyry) samples, (b) the relationship between MgO and SiO2, (c) the relationship between Zr and SiO2, (d) the relationship between Nb and SiO2, (E) the relationship between SR and SiO2, (f) the relationship between SR / Y and y (5) Chondrite normalized REE model and primitive mantle normalized trace element spider diagram of Chizhou granodiorite (porphyry) samples (6) Nd Sr isotopic map of intrusive rocks in Chizhou area (7) Zircon U-Pb dating of Chizhou intrusion (8) (a) lgfio2 and t (℃) of zircon samples and (b) Ce4 + / Ce3 of zircon samples ± (c) logfio2 and EU / EU * values of apatite samples from Chizhou intrusive rocks δ The curve of EU. MH: magnetite hematite buffer, FMQ: forsterite magnet quartz buffer, IW: Iron floating buffer (9) The (a) Ta / SM vs. TA, (b) V vs. Rb, (c) La / Yb vs. SiO2 curves of Chizhou granodiorite (porphyry) samples. Note: PM partial melting, FC fractional crystallization
XIE Jiancheng
The micrographs of granodiorite (porphyry) and molybdenite in Chizhou area include pailou granodiorite, Mashi granodiorite (porphyry), Xishan granodiorite and Matou molybdenite. The granodiorite (porphyry) in Chizhou area is gray white, granular (porphyry) structure and massive structure. They are mainly composed of quartz (20 – 25%), potash feldspar (20 – 25%), plagioclase (40 – 45%), amphibole (∼ 5%), biotite (∼ 10%), and accessory minerals such as zircon and apatite (Fig. 5a-d). Molybdenite is characterized by euhedral dihedral structure and occurs in vein, disseminated and nodular forms in quartz veins.
XIE Jiancheng
This data includes three maps: (a) tectonic map of China; (b) geological map of Late Mesozoic Magmatic Rocks and related deposits in the middle and lower reaches of the Yangtze River metallogenic belt; (c) geological map of Chizhou mining area in eastern China. The information in the map includes regional fault distribution, study area location, porphyry stratabound Cu Au Mo deposit, skarn Fe Cu deposit, magnetite apatite deposit, A-type granite belt, Cretaceous volcanic and subvolcanic rocks, late Mesozoic granodiorite and granite. Based on the systematic geochronological and geochemical analysis of the Cu Mo polymetallic deposits in the Ma'anshan fault zone and gaotan fault zone in the East Liuzhou area, the paper makes a deep study on the formation of Cu Mo polymetallic deposits and the genesis of granodiorite (porphyry) in Chizhou area. The above data are published in high-level SCI journals, and the data are true and reliable. The data is stored in JPG format.
XIE Jiancheng
The data include Re Os isotopic age of Molybdenite in Chizhou copper molybdenum deposit The Re Os isotopic composition of molybdenite was determined by tjax ICP-MS. Experimental characteristics of Re Os isotopic age: the uncertainty of each age measurement is about 1.5%, including the uncertainty of 187Re decay constant, the uncertainty of isotope ratio measurement and peak calibration. The decay constant is λ ( 187Re）=1.666 × 10-11 year−1。 According to the above rules, the final chronological data are formed. The above data have been published in SC journals, and the data are true and reliable. The uploaded data is in Excel format.
XIE Jiancheng
The data include nd, Sr isotopic compositions and la-mc-icp-ms zircon Hf isotopic compositions of granodiorite (porphyry) in Chizhou area. RB Sr and SM Nd isotopic data were measured at the laboratory of radiogenic isotope geochemistry, University of science and technology of China, using finnigan-mat-262 thermal ionization mass spectrometer. The Lu Hf isotopic composition of zircons was measured by 193 nm laser on Neptune multi collector ICP-MS (la-mc-icp-ms) at the State Key Laboratory of mineral deposit research, Nanjing University. The above data have been published in SCI high-level journals, and the data are true and reliable. The data is uploaded through Excel.
XIE Jiancheng
In Chizhou area, the whole rock of granodiorite (porphyry) is analyzed, and the major and trace elements are calculated. The table of geochemical results includes the results of chemical analysis of major elements and trace elements, as well as the data of whole rock δ EU and δ CE value analysis results. among δ EU and δ The calculation formula of CE value is δ Eu=EuN/(SmN × GdN)1/2, δ Ce=2Ce/(La+Pr) The main and trace elements were measured by X-ray fluorescence method, and the trace elements and rare earth elements were analyzed by ICP-MS. The data is uploaded in Excel form.
XIE Jiancheng
In Chizhou area, the accessory mineral apatite in the sample granodiorite (porphyry) was extracted and screened, and its major and trace element compositions were calculated. The table of geochemical results includes the results of chemical analysis of major elements and trace elements, as well as the data of whole rock δ EU and δ CE value analysis results. among δ EU and δ The calculation formula of CE value is δ Eu=EuN/(SmN × GdN)1/2, δ Ce=2Ce/(La+Pr) The main elements test site is located in the school of resources and environmental engineering, Hefei University of technology. The experimental instrument is jeol-jxa-8230m electron probe. LA-ICP-MS was used as analytical instrument in the State Key Laboratory of isotope geochemistry, Guangzhou Institute of geochemistry, Chinese Academy of Sciences. The above data have been published in SCI high-level journals, and the data are true and reliable. The data is uploaded in Excel form.
XIE Jiancheng
The table includes the results of zircon geochronology and trace element geochemistry of granodiorite (porphyry) in Chizhou area. The experimental method was la-icp-ms. The U-Pb isotopic composition of zircon was analyzed by Agilent 7500a ICP-MS instrument and compexpro 102193nm ArF excimer laser source in school of resource and environmental engineering, Hefei University of technology. The laser energy of 80 MJ and repetition rate of 6 Hz are used, and the frequency is 32 μ M spot size and 50 second ablation time. The isotopic ratios of zircons were calculated by ICP msdatacalv. This data can provide data support for future geochemical model analysis of granodiorite (porphyry) in Chizhou area. The above data have been published in SCI high-level journals, and the data are true and reliable. The data is stored in Excel.
XIE Jiancheng
This data includes excel and JPG format chart. Excel data include the contents and isotopic ratios of major and trace elements, Rb Sr and SM nd in the whole rock. All samples were crushed to less than 200 mesh using conventional techniques. The whole rock macro and trace element analysis was carried out in ALS minerals / ALS Chemex laboratory, Guangzhou, China. The contents and isotopic ratios of Rb Sr and SM nd were determined by isotope dilution method at the Key Laboratory of crust mantle materials and environment, University of science and technology of China. Jpg image format data include: (1) field photos and micrographs (cross polarized light) of Zhangbaling and Feidong intrusive rocks（ 2) Cathodoluminescence (CL) images of typical zircons from Zhangbaling intrusive rocks（ 3) Simplified geological map of the study area (a) the study area and its surrounding areas (b) the study area includes Zhangbaling and Feidong areas（ 4) Zircon U-Pb isotopic concordance map of Zhangbaling intrusion（ 5) Zircon U-Pb isotopic consistency map of Feidong intrusion（ 6) TAS igneous rock diagram (7) the relationship between MgO and SiO2 (a) and Mg # and SiO2 (b) (8) chondrite normalized REE model (9) Sr / Y and y) and (LA / Yb) n and YBN chart (10) Mesozoic Magmatic Rocks (LA / Yb) n and YBN of Zhangba formation represent LA / Yb and Yb normalized chondrite（ 11) The initial SR – Nd isotopic compositions of the late Mesozoic Magmatic Rocks of the Zhangba formation. Data of Dabie high Sr / y granitoids (12) initial isotopic composition of lead in Late Mesozoic (13) age distribution map of magmatic rocks in Zhangba formation (14) HF (T) and u – Pb age map of zircon intrusive rocks in Zhangba formation and data of rocks in other areas（ 15) Late Mesozoic Magmatic Rocks of Zhangba formation. This database can be used to study the deep crustal processes and tectonic relationships in the northern Zhangbaling and southeastern Feiling areas.
YAN Jun, LI Yixi
The data are zircon U-Pb data of volcanic rocks, major, trace and isotopic geochemical data of whole rock, and zircon Hf isotopic data. Samples were collected from basalt, basaltic andesite, andesite and dacite in the southern Lhasa terrane near sangyesi in Zedang area, southern Tibet. Radioisotope geochronology data were obtained by laser ablation inductively coupled plasma mass spectrometry and secondary ion probe analysis of zircon U-Pb isotopes. The major and trace geochemical data of the whole rock are obtained by X-ray fluorescence spectrometry and inductively coupled plasma mass spectrometry. The Hf isotopic data of zircons were obtained by laser ablation multiple acceptor plasma mass spectrometry. The age, origin and formation background of magmatism in the region can be defined by the data obtained.
ZHANG Liangliang
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