CCPortal
DOI10.1016/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
ISSN0040-1951
EISSN1879-3266
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
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).
条目包含的文件
条目无相关文件。
个性服务
推荐该条目
保存到收藏夹
导出为Endnote文件
谷歌学术
谷歌学术中相似的文章
[Yao, Wei]的文章
[Ding, Lin]的文章
[Cai, Fulong]的文章
百度学术
百度学术中相似的文章
[Yao, Wei]的文章
[Ding, Lin]的文章
[Cai, Fulong]的文章
必应学术
必应学术中相似的文章
[Yao, Wei]的文章
[Ding, Lin]的文章
[Cai, Fulong]的文章
相关权益政策
暂无数据
收藏/分享

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。