OIB-type rocks within West Junggar ophiolitic melanges: Evidence for the accretion of seamounts
文献类型：期刊论文
| 作者 | Yang, Gaoxue1,2; Li, Yongjun1,2; Xiao, Wenjiao3,4,5; Tong, Lili1,2 |
| 刊名 | EARTH-SCIENCE REVIEWS
 |
| 出版日期 | 2015-11-01 |
| 卷号 | 150页码:477-496 |
| 关键词 | Ophiolite Seamount Accretion Xinjiang Central Asian Orogenic Belt |
| DOI | 10.1016/j.earscirev.2015.09.002 |
| 文献子类 | Article |
| 英文摘要 | The Central Asian Orogenic Belt (CAOB, also known as the Altaid Tectonic Collage), one of the largest and long-lived accretionary orogens in the world, developed from ca. 600 Ma to 250 Ma by multiple accretions of terranes of different origin. Despite extensive research aimed at understanding tectonic evolution of the CAOB and the evolution of the Paleo-Asian Ocean, the subduction-accretion mechanism of the CAOB remains controversial. The West Junggar, northwestern China, is located in the southwest of the CAOB and consists of Paleozoic ophiolitic melanges, arcs and accretionary complexes. |
| WOS关键词 | ASIAN OROGENIC BELT ; PALEOZOIC TECTONIC EVOLUTION ; PHANEROZOIC CRUSTAL GROWTH ; NW CHINA IMPLICATIONS ; DAIICHI-KASHIMA SEAMOUNT ; TRACE-ELEMENT EVIDENCE ; MEXICAN VOLCANIC BELT ; ND ISOTOPIC EVIDENCE ; A-TYPE GRANITES ; CONTINENTAL GROWTH |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000364796200022 |
| 资助机构 | National Natural Science Foundation of China(41303027 ; National Natural Science Foundation of China(41303027 ; Special Fund for Basic Scientific Research of Central Colleges, Chang'an University(310827153506 ; Special Fund for Basic Scientific Research of Central Colleges, Chang'an University(310827153506 ; 41230207) ; 41230207) ; 310827153407 ; 310827153407 ; 2014G1271058) ; 2014G1271058) ; National Natural Science Foundation of China(41303027 ; National Natural Science Foundation of China(41303027 ; Special Fund for Basic Scientific Research of Central Colleges, Chang'an University(310827153506 ; Special Fund for Basic Scientific Research of Central Colleges, Chang'an University(310827153506 ; 41230207) ; 41230207) ; 310827153407 ; 310827153407 ; 2014G1271058) ; 2014G1271058) |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/62168]  |
| 专题 | 地质与地球物理研究所_岩石圈演化国家重点实验室 |
| 作者单位 | 1.Changan Univ, Sch Earth Sci & Resources, Xian 710054, Peoples R China 2.MLR, Key Lab Study Focused Magmatism & Giant Ore Depos, Xian 710054, Peoples R China 3.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 4.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China 5.Chinese Acad Sci, Xinjiang Res Ctr Mineral Resources, Xinjiang Inst Ecol & Geog, Urumqi 830011, Peoples R China |
| 推荐引用方式 GB/T 7714 | Yang, Gaoxue,Li, Yongjun,Xiao, Wenjiao,et al. OIB-type rocks within West Junggar ophiolitic melanges: Evidence for the accretion of seamounts[J]. EARTH-SCIENCE REVIEWS,2015,150:477-496. |
| APA | Yang, Gaoxue,Li, Yongjun,Xiao, Wenjiao,&Tong, Lili.(2015).OIB-type rocks within West Junggar ophiolitic melanges: Evidence for the accretion of seamounts.EARTH-SCIENCE REVIEWS,150,477-496. |
| MLA | Yang, Gaoxue,et al."OIB-type rocks within West Junggar ophiolitic melanges: Evidence for the accretion of seamounts".EARTH-SCIENCE REVIEWS 150(2015):477-496. |
入库方式： OAI收割
来源：地质与地球物理研究所
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