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DOI | 10.1016/j.tecto.2017.09.016 |
Origin and tectonic evolution of upper Triassic Turbidites in the Indo-Burman ranges, West Myanmar | |
Yao, Wei; Ding, Lin; Cai, Fulong; Wang, Houqi; Xu, Qiang; Zaw, Than | |
通讯作者 | Yao, W (通讯作者) |
发表日期 | 2017 |
ISSN | 0040-1951 |
EISSN | 1879-3266 |
起始页码 | 90 |
结束页码 | 105 |
卷号 | 721 |
英文摘要 | The Pane Chaung Formation is exposed in the Indo-Burman Ranges, and has been involved in collision between the Indian Plate and West Burma Block. However, controversies exist over the provenance and paleogeographic reconstruction of the Pane Chaung Formation. This study presents new petrographical and detrital zircon U-Pb ages and Hf isotopic data from the Pane Chaung Formation in Rakhine Yoma and Chin Hills, west Myanmar. The depositional age of the Pane Chaung Formation is Late Triassic, indicated by the Carnian-Norian Halobia fossils and maximum depositional ages between 233.0 +/- 2.5 Ma and 206.2 +/- 1.8 Ma. Upper Triassic sandstones contain 290-200 Ma detrital zircons, epsilon Hf(t) values of 6 to 11 and TDMC of 1.6 to 0.6 Ga, interpreted to be derived from West Papua region. The most abundant zircon age population of 750-450 Ma is derived from Pan-African orogenic belts in Australia. Zircons of 1250-900 Ma age were derived from the Grenvillian orogen in Australia. Archean zircons are interpreted to be derived from the Yilgarn and Pilbara cratons in Western Australia. Detrital zircon ages of the Pane Chaung Formation are distinct from similar aged strata in Indochina and Sibumasu, but comparable to NW Australia (Carnarvon Basin) and Greater India (Langjiexue Formation). It is suggested that the Pane Chaung Formation was deposited in a Late Triassic submarine fan along the northern margin of Australia. |
关键词 | MOGOK METAMORPHIC BELTNEW-ENGLAND BATHOLITHU-PB GEOCHRONOLOGYDETRITAL ZIRCONSHF-ISOTOPESEASTERN AUSTRALIANORTHWARD MIGRATIONSOUTHEAST-ASIATRACE-ELEMENTSHAN SCARP |
英文关键词 | Pane Chaung formation; Upper Triassic turbidites; Indo-Burman ranges; Provenance; Paleogeographic reconstruction |
语种 | 英语 |
WOS研究方向 | Geochemistry & Geophysics |
WOS类目 | Geochemistry & Geophysics |
WOS记录号 | WOS:000418309400007 |
来源期刊 | TECTONOPHYSICS
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来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/258915 |
推荐引用方式 GB/T 7714 | Yao, Wei,Ding, Lin,Cai, Fulong,et al. Origin and tectonic evolution of upper Triassic Turbidites in the Indo-Burman ranges, West Myanmar[J]. 中国科学院青藏高原研究所,2017,721. |
APA | Yao, Wei,Ding, Lin,Cai, Fulong,Wang, Houqi,Xu, Qiang,&Zaw, Than.(2017).Origin and tectonic evolution of upper Triassic Turbidites in the Indo-Burman ranges, West Myanmar.TECTONOPHYSICS,721. |
MLA | Yao, Wei,et al."Origin and tectonic evolution of upper Triassic Turbidites in the Indo-Burman ranges, West Myanmar".TECTONOPHYSICS 721(2017). |
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