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
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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-+. |
入库方式: OAI收割
来源:地质与地球物理研究所
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