Geochronology and petrogenesis of granitic rocks in Gangdese batholith, southern Tibet | |
Ji WeiQiang1,2; Wu FuYuan1; Liu ChuanZhou1; Chung SunLin3 | |
刊名 | SCIENCE IN CHINA SERIES D-EARTH SCIENCES
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2009-09-01 | |
卷号 | 52期号:9页码:1240-1261 |
关键词 | Tibet Gangdese batholith granitic rock geochronology petrogenesis |
ISSN号 | 1006-9313 |
DOI | 10.1007/s11430-009-0131-y |
文献子类 | Review |
英文摘要 | Based on petrological and geochemical characteristics such as rock assemblage, petrogeochemistry, Sr-Nd isotope, zircon U-Pb age, and Hf isotope, we studied geochronological framework, magma types, source characters, and petrogenesis of different stages of magmatism of the granitic rocks from the Gangdese batholith in southern Tibet. The magmatic activities of the Gangdese batholith can be divided into three stages. The Mesozoic magmatism, induced by northern subduction of Neotethyan slab, was continuously developed, with two peak periods of Late Jurassic and Early Cretaceous. The Paleocene-Eocene magmatism was the most intensive, and resulted from a complex progress of Neotethyan oceanic slab, including subduction, rollback, and subsequent breakoff. And the Oligocene-Miocene magmatism was attributed to the convective removal of thickened lithosphere in an east-west extension setting after India-Asia collision. Isotopically, zircons from these granitic rocks are characterized by positive E > (Hf)(t) values, suggesting that the magmatic source of the Gangdese batholith might be an arc terrane, which was accreted to the southern margin of Asia during Late Paleozoic. Therefore, the chronological framework and Hf isotopic characteristics of the Gangdese batholith are distinct from the granitic rocks in adjacent areas, which can be served as a powerful tracer in studying source-to-sink relation of sediments during the uplift and erosion of Tibetan Plateau. |
WOS关键词 | INDIA-ASIA COLLISION ; ZIRCON U-PB ; TSANGPO SUTURE ZONE ; FORE-ARC BASIN ; EAST-WEST EXTENSION ; VOLCANIC-ROCKS ; CONTINENTAL COLLISION ; TECTONIC EVOLUTION ; EURASIA COLLISION ; LHASA BLOCK |
WOS研究方向 | Geology |
语种 | 英语 |
出版者 | SCIENCE PRESS |
WOS记录号 | WOS:000269974200002 |
资助机构 | Chinese Academy of Sciences(KZCX2-YW-Q09-06) ; Chinese Academy of Sciences(KZCX2-YW-Q09-06) ; Chinese Academy of Sciences(KZCX2-YW-Q09-06) ; Chinese Academy of Sciences(KZCX2-YW-Q09-06) ; National Natural Science Foundation of China(40721062) ; National Natural Science Foundation of China(40721062) ; National Natural Science Foundation of China(40721062) ; National Natural Science Foundation of China(40721062) ; Chinese Academy of Sciences(KZCX2-YW-Q09-06) ; Chinese Academy of Sciences(KZCX2-YW-Q09-06) ; Chinese Academy of Sciences(KZCX2-YW-Q09-06) ; Chinese Academy of Sciences(KZCX2-YW-Q09-06) ; National Natural Science Foundation of China(40721062) ; National Natural Science Foundation of China(40721062) ; National Natural Science Foundation of China(40721062) ; National Natural Science Foundation of China(40721062) ; Chinese Academy of Sciences(KZCX2-YW-Q09-06) ; Chinese Academy of Sciences(KZCX2-YW-Q09-06) ; Chinese Academy of Sciences(KZCX2-YW-Q09-06) ; Chinese Academy of Sciences(KZCX2-YW-Q09-06) ; National Natural Science Foundation of China(40721062) ; National Natural Science Foundation of China(40721062) ; National Natural Science Foundation of China(40721062) ; National Natural Science Foundation of China(40721062) ; Chinese Academy of Sciences(KZCX2-YW-Q09-06) ; Chinese Academy of Sciences(KZCX2-YW-Q09-06) ; Chinese Academy of Sciences(KZCX2-YW-Q09-06) ; Chinese Academy of Sciences(KZCX2-YW-Q09-06) ; National Natural Science Foundation of China(40721062) ; National Natural Science Foundation of China(40721062) ; National Natural Science Foundation of China(40721062) ; National Natural Science Foundation of China(40721062) |
内容类型 | 期刊论文 |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/70382] ![]() |
专题 | 中国科学院地质与地球物理研究所 |
通讯作者 | Wu FuYuan |
作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 2.Chinese Acad Sci, Grad Univ, Beijing 100049, Peoples R China 3.Taiwan Natl Univ, Dept Geosci, Taipei 106, Taiwan |
推荐引用方式 GB/T 7714 | Ji WeiQiang,Wu FuYuan,Liu ChuanZhou,et al. Geochronology and petrogenesis of granitic rocks in Gangdese batholith, southern Tibet[J]. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,2009,52(9):1240-1261. |
APA | Ji WeiQiang,Wu FuYuan,Liu ChuanZhou,&Chung SunLin.(2009).Geochronology and petrogenesis of granitic rocks in Gangdese batholith, southern Tibet.SCIENCE IN CHINA SERIES D-EARTH SCIENCES,52(9),1240-1261. |
MLA | Ji WeiQiang,et al."Geochronology and petrogenesis of granitic rocks in Gangdese batholith, southern Tibet".SCIENCE IN CHINA SERIES D-EARTH SCIENCES 52.9(2009):1240-1261. |
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