中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Early Cretaceous wedge extrusion in the Indo-Burma Range accretionary complex: implications for the Mesozoic subduction of Neotethys in SE Asia

文献类型:期刊论文

作者Zhang, JE (Zhang, Ji'en)1; Xiao, WJ (Xiao, Wenjiao)1,2,3; Windley, B (Windley, Brian F.)4; Cai, FL (Cai, Fulong)5; Sein, K (Sein, Kyaing)6; Naing, S (Naing, Soe)6; Zhang, JE
刊名INTERNATIONAL JOURNAL OF EARTH SCIENCES
出版日期2018
卷号106期号:4页码:1391-1408
关键词MANIPUR OPHIOLITE COMPLEX MYANMAR OROGENIC BELT ZIRCON U-PB NORTHEAST INDIA NAGA HILLS TECTONIC EVOLUTION WESTERN MYANMAR EMPLACEMENT HISTORY PLATE STRATIGRAPHY SOUTHEAST-ASIA
DOI10.1007/s00531-017-1468-7
文献子类Article; Proceedings Paper
英文摘要The Indo-Burma Range (IBR) of Myanmar, the eastern extension of the Yarlung-Tsangpo Neotethyan belt of Tibet in China, contains m,langes with serpentinite, greenschist facies basalt, chert, sericite schist, silty slate and unmetamorphosed Triassic sandstone, mudstone and siltstone interbedded with chert in the east, and farther north high-pressure blueschist and eclogite blocks in the Naga Hills m,lange. Our detailed mapping of the Mindat and Magwe sections in the middle IBR revealed a major similar to 18 km antiformal isocline in a m,lange in which greenschist facies rocks in the core decrease in grade eastwards and westwards symmetrically 'outwards' to lower grade sericite schist and silty slate, and at the margins to unmetamorphosed sediments, and these metamorphic rocks are structurally repeated in small-scale imbricated thrust stacks. In the Mindat section the lower western boundary of the isoclinal m,lange is a thrust on which the metamorphic rocks have been transported over unmetamorphosed sediments of the Triassic Pane Chaung Group, and the upper eastern boundary is a normal fault. These relations demonstrate that the IBR metamorphic rocks were exhumed by wedge extrusion in a subduction-generated accretionary complex. Along strike to the north in the Naga Hills is a comparable isoclinal m,lange in which central eclogite lenses are succeeded 'outwards' by layers of glaucophane schist and glaucophanite, and to lower grade greenschist facies sericite schist and slate towards the margins. In the Natchaung area (from west to east) unmetamorphosed Triassic sediments overlie quartzites, sericite schists, actinolite schists and meta-volcanic amphibolites derived from MORB-type basalt, which are in fault contact with peridotite. Olivine in the peridotite has undulatory extinction suggesting deformation at 600-700 A degrees C, similar to the peak temperature of the amphibolite; these relations suggest generation in a metamorphic sole. The amphibolites have U/Pb zircon ages of 119 +/- 3 Ma and 115 Ma, which are close to the zircon ages of nearby calc-alkaline granite and diorite, which belong to an active continental margin arc that extends along the western side of the Shan-Thai block. The IBR accretionary complex and the active continental margin arc were generated during Early Cretaceous (115-128 Ma) subduction of the Neotethys Ocean.
学科主题地质学
WOS研究方向Geology
语种英语
WOS记录号WOS:000401629200013
源URL[http://ir.itpcas.ac.cn/handle/131C11/8230]  
专题青藏高原研究所_图书馆
通讯作者Zhang, JE
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Tethys Res Ctr, Beijing 100029, Peoples R China.
2.Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China.
3.Chinese Acad Sci, Xinjiang Inst Ecol & Geog, Xinjiang Res Ctr Mineral Resources, Urumqi 830011, Peoples R China.
4.Univ Leicester, Dept Geol, Leicester LE1 7RH, Leics, England.
5.Inst Tibetan Plateau Res, Key Lab Continental Collis & Plateau Uplift, Beijing 100101, Peoples R China.
6.Myanmar Geosci Soc, Yangon, Myanmar.
推荐引用方式
GB/T 7714
Zhang, JE ,Xiao, WJ ,Windley, B ,et al. Early Cretaceous wedge extrusion in the Indo-Burma Range accretionary complex: implications for the Mesozoic subduction of Neotethys in SE Asia[J]. INTERNATIONAL JOURNAL OF EARTH SCIENCES,2018,106(4):1391-1408.
APA Zhang, JE .,Xiao, WJ .,Windley, B .,Cai, FL .,Sein, K .,...&Zhang, JE.(2018).Early Cretaceous wedge extrusion in the Indo-Burma Range accretionary complex: implications for the Mesozoic subduction of Neotethys in SE Asia.INTERNATIONAL JOURNAL OF EARTH SCIENCES,106(4),1391-1408.
MLA Zhang, JE ,et al."Early Cretaceous wedge extrusion in the Indo-Burma Range accretionary complex: implications for the Mesozoic subduction of Neotethys in SE Asia".INTERNATIONAL JOURNAL OF EARTH SCIENCES 106.4(2018):1391-1408.

入库方式: OAI收割

来源:青藏高原研究所

浏览0
下载0
收藏0
其他版本

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。