The Indosinian orogenesis occurred in Lhasa terrain and the evidence from muscovite Ar-40-Ar-39 geochronology | |
Li, HQ (Li HuaQi); Cai, ZH (Cai ZhiHui); Chen, SY (Chen SongYong); Tang, ZM (Tang ZheMin); Yang, M (Yang Mei) | |
刊名 | ACTA PETROLOGICA SINICA
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2008 | |
卷号 | 24期号:7页码:1595-1604 |
关键词 | Lhasa terrain Eclogite Ductile shearing belt Ar-40-Ar-39 geochronology Indosinian orogenesis |
ISSN号 | 1000-0569 |
英文摘要 | Based on the the deformation characteristic of Sumdo Group and the ductile shearing zones, the quartz fabric by EBSD, the data of muscovite Ar-40-Ar-39 geochronology (220 similar to 230Ma) from ductile shearing zones and the large scale granite of Late Triassic epoch in Sumdo Group, Lhasa terrain is thought to have experienced an important Indosinian orogenic event, which caused the closure of the Paleo-Tethys ocean along the tectonic zone of eclogite and the collision between northern part and Southern part of Lhasa terrain. The discovery of Indosinian orogenic belt in Lhasa terrain expanse the southern boundary of Indosinian orogenie belt to Lhasa terrain from Qiangtang terrain, which is very important to the research of the Paleo-Tethys ocean along Tibet. |
学科主题 | 构造地质学 |
WOS研究方向 | Geology |
语种 | 中文 |
出版者 | SCIENCE CHINA PRESS |
WOS记录号 | WOS:000260313300015 |
内容类型 | 期刊论文 |
源URL | [http://119.78.100.197/handle/2HKVOGP0/38727] ![]() |
专题 | 中国地质调查局 |
作者单位 | Chinese Acad Geol Sci, Inst Hydrogeol & Environm Geol, Shijiazhuang 050061, Peoples R China |
推荐引用方式 GB/T 7714 | Li, HQ ,Cai, ZH ,Chen, SY ,et al. The Indosinian orogenesis occurred in Lhasa terrain and the evidence from muscovite Ar-40-Ar-39 geochronology[J]. ACTA PETROLOGICA SINICA,2008,24(7):1595-1604. |
APA | Li, HQ ,Cai, ZH ,Chen, SY ,Tang, ZM ,&Yang, M .(2008).The Indosinian orogenesis occurred in Lhasa terrain and the evidence from muscovite Ar-40-Ar-39 geochronology.ACTA PETROLOGICA SINICA,24(7),1595-1604. |
MLA | Li, HQ ,et al."The Indosinian orogenesis occurred in Lhasa terrain and the evidence from muscovite Ar-40-Ar-39 geochronology".ACTA PETROLOGICA SINICA 24.7(2008):1595-1604. |
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