中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Upper Cretaceous-Lower Eocene Dajiweng Formation in the Zhada area, southern Tibet : Implications for the Trans-Himalayan forearc baisn evolution

文献类型:期刊论文

作者Sun GaoYuan1; Wang JianGang2; Hu XiuMian3; Boudagher-Fadal, Marcelle K.4
刊名ACTA PETROLOGICA SINICA
出版日期2018
卷号34期号:6页码:1847-+
关键词Eocene Sedimentary records Zircon U-Pb and Hf Forearc marine regression Forearc basin
ISSN号1000-0569
英文摘要The marine strata in the Gangdese forearc area play a significant role in the study of the closure of Neo-Tethyan Ocean and the subsequent India-Asia collision. The Dajiweng Formation exposed in the Zhada area, southern Tibet, is bounded by the southern Gangdese magmatic arc to the north and the Indus-Yarlung Zangbo suture zone to the south. It is mainly composed of conglomerate, sandstone, mudstone and limestone. Sedimentary analysis revealed that the Dajiweng Formation had been deposited in the fan-delta environment. A combination of the tuff zircon U-Pb dating, youngest detrital zircon ages and large benthic foraminiferal assemblage yielded that the Dajiweng Formation formed during the Late Cretaceous-Early Eocene period (i.e., ca. 73 similar to 49Ma). The provenance data showed that the Dajiweng Formation is similar to that of the Xigaze forearc basin sediments, which were mostly derived directly from the Gangdese magmatic arc. In contrast to the Gangdese-Ladakh forearc deposits, the forearc marine regression was diachronous along the strike, i.e. the sea water regressing gradually from east to west and disappearing at similar to 49 Ma in the western Gangdese-Ladakh forearc area.
WOS关键词ZIRCON U-PB ; FACIES ARCHITECTURE ; MAGMATIC EVOLUTION ; LADAKH HIMALAYA ; LU-HF ; BASIN ; GANGDESE ; PROVENANCE ; PETROGENESIS ; CONSTRAINTS
WOS研究方向Geology
语种英语
WOS记录号WOS:000451721000020
出版者SCIENCE PRESS
源URL[http://ir.iggcas.ac.cn/handle/132A11/89627]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Wang JianGang
作者单位1.Hohai Univ, Coll Oceanog, Nanjing 210098, Jiangsu, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
3.Nanjing Univ, Sch Earth Sci & Engn, State Key Lab Mineral Deposits Res, Nanjing 210023, Jiangsu, Peoples R China
4.UCL, Dept Earth Sci, London WC1H 0BT, England
推荐引用方式
GB/T 7714
Sun GaoYuan,Wang JianGang,Hu XiuMian,et al. Upper Cretaceous-Lower Eocene Dajiweng Formation in the Zhada area, southern Tibet : Implications for the Trans-Himalayan forearc baisn evolution[J]. ACTA PETROLOGICA SINICA,2018,34(6):1847-+.
APA Sun GaoYuan,Wang JianGang,Hu XiuMian,&Boudagher-Fadal, Marcelle K..(2018).Upper Cretaceous-Lower Eocene Dajiweng Formation in the Zhada area, southern Tibet : Implications for the Trans-Himalayan forearc baisn evolution.ACTA PETROLOGICA SINICA,34(6),1847-+.
MLA Sun GaoYuan,et al."Upper Cretaceous-Lower Eocene Dajiweng Formation in the Zhada area, southern Tibet : Implications for the Trans-Himalayan forearc baisn evolution".ACTA PETROLOGICA SINICA 34.6(2018):1847-+.

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来源:地质与地球物理研究所

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