The data are the whole rock major and trace element data, zircon U-Pb dating data, zircon Lu Hf isotopic data, and silicate melt inclusion data of diamond bearing alkaline basalt in balustrade area, China. The major element data of the whole rock were obtained by XRF analysis, the trace element data were obtained by ICP-MS analysis, and the zircon U-Pb dating and in-situ Lu Hf isotopic composition data were obtained by la-mc-icp-ms analysis. The data of silicate melt inclusions were obtained by LA-ICP-MS analysis. The above data have been published in high-level SCI journals, and the data are true and reliable. The research results have certain guiding significance for limiting the initial failure time and possible mechanism of NCC.
XIAO Yilin
This data is the major and trace elements of Cretaceous monzonite, biotite, zircon U-Pb isotopic dating data and zircon Lu Hf isotopic data in Chuzhou area of the lower Yangtze River metallogenic belt. The major element data of the whole rock were obtained by XRF analysis, the trace element data were obtained by ICP-MS analysis, and the zircon U-Pb dating and in-situ Lu Hf isotopic composition data were obtained by la-mc-icp-ms analysis. The major elements of biotite were obtained by EPMA analysis. The above data have been published in high-level SCI journals, and the data are true and reliable. Through the data obtained, we can better understand the petrogenesis and put forward more solid constraints on the geological evolution of the Qinghai Tibet Plateau.
YANG Xiaoyong
The data include the stable isotope data of elements and metals of a series of Cretaceous rocks in the Dabie orogenic belt, as well as a small number of hand specimen photos and micrographs. X-ray fluorescence spectrometry (XRF) was used to test the major elements with an accuracy of less than 2%, inductively coupled plasma mass spectrometry (ICP-MS) was used to test the trace elements with an accuracy of less than 5%, and multi-channel inductively coupled plasma mass spectrometry (MC-ICPMS) was used to test the stable isotopes of Ca, Mg and Fe with an accuracy of more than 0.06 ‰. The above tests were completed from May 14, 2016 to June 19, 2020, The data have been published in many international well-known petrological journals, such as geochimica et cosmochimica Acta, chemical geology, etc. These data are of great significance for understanding the fractionation behavior of metal stable isotopes in magmatic rock systems.
WU Hongjie
Contact Support
Northwest Institute of Eco-Environment and Resources, CAS
0931-4967287
poles@itpcas.ac.cn
Links
National Tibetan Plateau Data CenterFollow Us
A Big Earth Data Platform for Three Poles © 2018-2020 No.05000491 | All Rights Reserved
｜ 
No.11010502040845
Tech Support: westdc.cn
