Research on SHRIMP U-Pb chronology in Xiaoqinling-Xionger' shan area: the evidence of delamination of lithosphere in Qinling orogenic belt | |
Wang, TH (Wang TuanHua); Mao, JW (Mao JingWen); Wang, YB (Wang YanBin) | |
刊名 | ACTA PETROLOGICA SINICA
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2008 | |
卷号 | 24期号:6页码:1273-1287 |
关键词 | dike chronology of zircon SHRIMP IIU-Pb dating delamination Xiaoqinling-Xiong' ershan area Qinling orogenic belt Southern of North China craton |
ISSN号 | 1000-0569 |
英文摘要 | Chronology research by SHRIMP II U-Pb dating on zircon from dikes of Xiaoqinling-Xiong' ershan area show that the zircons in dike magmas source mainly are inherited ones, which manifest chronologic characteristics of Southern edge of North China continental basement. The two dikes which have definite geological relation that invaded into granite of Mesozoic epoch may give the dating results of 1843 +/- 10Ma and 768 +/- 15Ma, and most zircon show the time of 1850Ma for a very large scale volcanic activity events of Xiong' er group in the region, only few of zircon show the reasonable time of 128Ma in Mesozoic epoch. To view the chronologic data as a whole, the zircons in dikes comprehensively record the regional history of tectonic evolution. The results of zircon dating reflected the tectonic and magmas events in North China craton as Fuping movement (2500 similar to 2400Ma), volcanic eruption activity of Xionger' group in Southern edge of North China craton (1850Ma), Paleo-Sinian tectonic movement (850 similar to 700Ma) and succession events of orogen process (similar to 200Ma) and dike magmas invading events(similar to 130Ma) with Yangtze plate subducted and matched to Southern edge of North China craton. Research on tracing of Sr, Nd, Pb of dikes reveal that the magmas source of dikes have much affinity to Yangtze Plate, the fact testified the dynamic process of Yangtze plate subduction to Southern edge of North China craton from Neo-Priterozoic to Pilo-Paleozoic time and delamination of continental low Crust of Qinling orogenic belt in Southern edge of North China in post of orogen in the late. The reason for most of dating results of zircon in dikes show the characteristics of inherited one possibly is that the zircon grain grow small in Mesozoic epoch, but the inherit zircons grain are bigger than the zircon in Mesozoic, so that most of inherit zircon were selected during mineral sorting but Mesozoic zircon were difficult to be selected out. |
学科主题 | 固体地球物理学 |
WOS关键词 | NORTH CHINA ; GEODYNAMIC SETTINGS ; DEPOSITS ; AGES |
WOS研究方向 | Geology |
语种 | 中文 |
出版者 | SCIENCE CHINA PRESS |
WOS记录号 | WOS:000259628800010 |
内容类型 | 期刊论文 |
源URL | [http://119.78.100.197/handle/2HKVOGP0/38636] ![]() |
专题 | 中国地质调查局 |
作者单位 | Chinese Acad Geol Sci, Inst Geol, Beijing 100037, Peoples R China |
推荐引用方式 GB/T 7714 | Wang, TH ,Mao, JW ,Wang, YB . Research on SHRIMP U-Pb chronology in Xiaoqinling-Xionger' shan area: the evidence of delamination of lithosphere in Qinling orogenic belt[J]. ACTA PETROLOGICA SINICA,2008,24(6):1273-1287. |
APA | Wang, TH ,Mao, JW ,&Wang, YB .(2008).Research on SHRIMP U-Pb chronology in Xiaoqinling-Xionger' shan area: the evidence of delamination of lithosphere in Qinling orogenic belt.ACTA PETROLOGICA SINICA,24(6),1273-1287. |
MLA | Wang, TH ,et al."Research on SHRIMP U-Pb chronology in Xiaoqinling-Xionger' shan area: the evidence of delamination of lithosphere in Qinling orogenic belt".ACTA PETROLOGICA SINICA 24.6(2008):1273-1287. |
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