Geochemistry of Punctuated orogeny during the assembly of Asia: Tectonostratigraphic evolution of the North China craton and the Qilian Shan from Paleoproterozoic to Early Paleozoic

Abstract: Whole rock geochemistry from the northern Tibetan Plateau, eastern Qilian Shan and Longshoushan. Samples range in age from Paleozoic to Proterozoic. Granitoid and volcanic rock samples were analyzed for major and trace elements at the Chinese Academy of Geologic Sciences in Beijing, China. Major elements were analyzed using an X-ray fluorescence spectrometer. Trace elements were measured on an inductively coupled plasma-mass spectrometry (ICP-MS).

Other Description: Wu, C., Zuza, A.V., Yin, A., Chen, X.H., Haproff, P.J., Li, J., Li, B., Ding, L., (2020). Punctuated orogeny during the assembly of Asia: Tectonostratigraphic evolution of the North China craton and the Qilian Shan from Paleoproterozoic to Early Paleozoic. Tectonics (in revision)

摘要：青藏高原北部、祁连山东部及龙首山地区的全岩地球化学数据。样品形成时代从古生代至元古宙。在中国北京的中国地质科学院，对花岗质岩石与火山岩样品开展了主量元素与微量元素分析。主量元素采用X射线荧光光谱仪（X-ray fluorescence spectrometer）进行测试，微量元素则通过电感耦合等离子体质谱法（ICP-MS）完成测定。

其他说明：Wu C.、Zuza A.V.、Yin A.、Chen X.H.、Haproff P.J.、Li J.、Li B.、Ding L.（2020年）。《亚洲聚合过程中的幕式造山作用：从古元古代至早古生代华北克拉通与祁连山的构造-地层演化》，刊载于《Tectonics》（已修回待刊）