The constituents of the Qingdao Yankou high to ultrahigh-pressure tectonic melange and their deformations
文献类型:期刊论文
作者 | Fang, AM; Zhao, ZY |
刊名 | ACTA PETROLOGICA SINICA
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出版日期 | 2004-09-01 |
卷号 | 20期号:5页码:1087-1096 |
关键词 | Yankou Su-lu High- To ultraHigh-pressure Belt Tectonic Melange Deformations Structural Styles And Stages |
ISSN号 | 1000-0569 |
文献子类 | Article |
英文摘要 | A high- to ultra high pressure (HP-UHP) metamorphic slab resulted from deep continental subduction and subsequent exhumation is well exposed in Yankou, northeastern Qingdao in the Sulu orogenic belt, China. It consists of two kinds of structural units, namely structurally coherent unit and non-coherent unit (UHP ductile shear melange), respectively. Similar to the ultrahigh-pressure metamorphic (UHPM) rocks at other localities in the Su-Lu UHPM belt, the coherent unit consists of interlayered granitic gneiss, paragneisses, retrograde eclogite and ultramafic rocks in which coesite and other UHP minerals are widely preserved, indicating that they have an UHP metamorphic history. While the later is a ductile shear complex that consists of highly sheared mylonitic matrix and weakly deformed blocks, of which the matrix is composed of interlayered granitic and eclogitic mylonites; while the blocks are granitoids and gabbro that are metamorphosed to a variable degree of coesite eclogite facies. The two units are separated by an ultramylonite zone of 20 similar to 30 cm wide, and the non-coherent unit structurally lies below the coherent one. |
WOS关键词 | COESITE-BEARING ECLOGITES ; CENTRAL CHINA ; EASTERN CHINA ; METAMORPHIC ROCKS ; YANGTZE CRATONS ; DABIE MOUNTAINS ; NORTH CHINA ; TERRANE ; EXHUMATION ; ZIRCON |
WOS研究方向 | Geology |
语种 | 英语 |
WOS记录号 | WOS:000224589100007 |
出版者 | SCIENCE CHINA PRESS |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/64509] ![]() |
专题 | 中国科学院地质与地球物理研究所 |
通讯作者 | Fang, AM |
作者单位 | Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China |
推荐引用方式 GB/T 7714 | Fang, AM,Zhao, ZY. The constituents of the Qingdao Yankou high to ultrahigh-pressure tectonic melange and their deformations[J]. ACTA PETROLOGICA SINICA,2004,20(5):1087-1096. |
APA | Fang, AM,&Zhao, ZY.(2004).The constituents of the Qingdao Yankou high to ultrahigh-pressure tectonic melange and their deformations.ACTA PETROLOGICA SINICA,20(5),1087-1096. |
MLA | Fang, AM,et al."The constituents of the Qingdao Yankou high to ultrahigh-pressure tectonic melange and their deformations".ACTA PETROLOGICA SINICA 20.5(2004):1087-1096. |
入库方式: OAI收割
来源:地质与地球物理研究所
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