气候变化领域集成服务门户(CCPortal): Provenance and tectonic evolution of Lower Paleozoic-Upper Mesozoic strata from Sibumasu terrane, Myanmar

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DOI	10.1016/j.gr.2015.03.005
	Provenance and tectonic evolution of Lower Paleozoic-Upper Mesozoic strata from Sibumasu terrane, Myanmar
	Cai, Fulong; Ding, Lin; Yao, Wei; Laskowski, Andrew K.; Xu, Qiang; Zhang, Ji'en; Sein, Kyaing
通讯作者	Cai, FL (通讯作者)
发表日期	2017
ISSN	1342-937X
EISSN	1878-0571
起始页码	325
结束页码	336
卷号	41
英文摘要	The provenance of Sibumasu terrane sedimentary rocks and their tectonic relationships with surrounding terranes exposed in Southeast Asia record separation and accretion of Gondwana-derived terranes during Late Paleozoic and Mesozoic time. This paper reports sandstone petrographic and U-Pb detrital zircon geochronologic data from Ordovician to Lower Jurassic strata within the Sibumasu terrane in Shan State, Myanmar. The Ordovician strata are composed of limestone and siltstone. The Lower Silurian Linwe and Upper Silurian Namhism Formations are comprised of limestone, silty sandstone, conglomerate and sandstone, respectively. Sandstones from both Ordovician and Silurian strata are dominated by 567-470 Ma and 982-917 Ma detrital zircons that are interpreted to be sourced from the eastern Gondwana supercontinent. The Carboniferous unit is composed of metasedimentary rocks (phyllite, slate, quartzite, and meta-marl). Sandstones from Carboniferous units show a strong 1165-1070 Ma detrital zircon age peak that is not present in the Ordovician and Silurian strata. These zircon grains were most likely derived from both the Albany-Fraser Province in Southwest Australia and Maud Province in Antarctic. The Upper Triassic to Lower Jurassic, shallow marine Loi-an Group consists of thin-to medium-bedded sandstone and mudstone that unconformably overly the Permian to Middle Triassic Plateau Limestone Group. Sandstones from the Loi-an Group contain abundant Permian to Triassic detrital zircons that are interpreted to have been derived from the Sukhothai Arc of the western Indochina terrane. Formation of this arc is attributed to eastward (present coordinates) subduction of Paleo-Tethyan oceanic lithosphere beneath Indochina. Therefore, we propose that the Sibumasu terrane was juxtaposed against northwestern Australia as part of the Gondwana supercontinent during Paleozoic to Early Permian time. During the Late Triassic and Early Jurassic, Sibumasu strata record an abrupt influx of Permian and Triassic zircon grains, signifying a change in provenance from Gondwana to the Sukhothai Arc. These data are consistent with a tectonic model involving rifting of the Sibumasu terrane from Gondwana and subsequent docking with the Indochina/Simao terranes during Mesozoic time. (C) 2015 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.
关键词	TRIASSIC RADIOLARIAN FAUNAS ARC/BACK-ARC ASSEMBLAGES ZIRCON U-PB DETRITAL ZIRCONS SOUTHEAST-ASIA HF-ISOTOPES GEOCHRONOLOGICAL CONSTRAINTS TIBET IMPLICATIONS EAST ANTARCTICA TETHYS OROGEN
英文关键词	Myanmar; Sibumasu terrane; Detrital zircon dating; Provenance analysis; Paleogeography; Collision
语种	英语
WOS研究方向	Geology
WOS类目	Geosciences, Multidisciplinary
WOS记录号	WOS:000397873300021
来源期刊	GONDWANA RESEARCH
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/259007
推荐引用方式 GB/T 7714	Cai, Fulong,Ding, Lin,Yao, Wei,et al. Provenance and tectonic evolution of Lower Paleozoic-Upper Mesozoic strata from Sibumasu terrane, Myanmar[J]. 中国科学院青藏高原研究所,2017,41.
APA	Cai, Fulong.,Ding, Lin.,Yao, Wei.,Laskowski, Andrew K..,Xu, Qiang.,...&Sein, Kyaing.(2017).Provenance and tectonic evolution of Lower Paleozoic-Upper Mesozoic strata from Sibumasu terrane, Myanmar.GONDWANA RESEARCH,41.
MLA	Cai, Fulong,et al."Provenance and tectonic evolution of Lower Paleozoic-Upper Mesozoic strata from Sibumasu terrane, Myanmar".GONDWANA RESEARCH 41(2017).