Devonian to Permian plate tectonic cycle of the Paleo-Tethys Orogen in southwest China (I): Geochemistry of ophiolites, arc/back-arc assemblages and within-plate igneous rocks | |
Jian, Ping1; Liu, Dunyi1; Kroener, Alfred2; Zhang, Qi3; Wang, Yizhao4; Sun, Xiaomeng5; Zhang, Wei1 | |
刊名 | LITHOS
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2009-12-01 | |
卷号 | 113期号:3-4页码:748-766 |
关键词 | Geochemistry Ophiolite Arc/back-arc assemblages Within-plate igneous rocks Paleo-Tethys Southwest China |
ISSN号 | 0024-4937 |
DOI | 10.1016/j.lithos.2009.04.004 |
文献子类 | Article |
英文摘要 | The Paleo-Tethys Orogen in southwest China is an amalgamation of continental terranes (Sibumasu, Simao and Yangtze), which are bounded by ophiolite belts (Ailaoshan, Jinshajiang and Changning-Menglian) that represent former ocean basins. This study concentrates on ophiolites, arc/back-arc assemblages, and within-plate igneous rocks that occur in this complex orogen. Mainly based on geochemical fingerprinting of basalts, the Paleo-Tethys ophiolites are here classified as MORB and SSZ types. The Ailaoshan ophiolite (NMORB-type; ca. 387-374 Ma) is associated with a non-volcanic segment of the rifted western Yangtze margin. The Jinshajiang ophiolite (EMORB-type; 346-341 Ma), which has ophiolite structure but some samples bear crustal contamination signatures, is associated with a volcanic segment of the rifted Yangtze western margin. These MORB-type ophiolites are interpreted to have formed in the continent-ocean transition zones. The Changning Menglian ophiolite, which marks the main Paleo-Tethys suture, that is, the boundary between the Gondwana-derived Sibumasu terrane and the Yangtze-derived Simao terrane, has traditionally been thought to have a mid-ocean ridge (MOR) origin. New trace element data of basalts, however, indicate that this ophiolite (ca. 270-264 Ma) was formed at a supra-subduction zone (SSZ). Arc and back-arc assemblages are represented by the Gicha (ca. 311-277 Ma) and Banpo (ca. 288-284 Ma) zoned mafic-ultramafic complexes and the Yaxianqiao arc volcanic rocks (ca. 268-264 Ma). Geochemical data suggest that the Gicha complex originated in a back-arc rift. The Banpo complex makes a plutonic arc that contains low-Ti gabbro and tonalite with volcanic arc granite (VAG) affinity. Within-plate igneous rocks are recognized as xenoliths (amphibolites; ca. 443-401 Ma) in the Jinshajinag ophiolite melange and the Dalongkai small differentiated mafic-ultramafic intrusion (ca. 247-244 Ma) that intruded the Yaxianqiao Arc. The amphibolite xenoliths are similar to low-Ti continental flood basalts (CFB) in composition. Rocks from the small mafic-ultramafic intrusion have superimposed subduction and within-plate geochemical signatures. These ophiolites, arc/back-arc assemblages and within-plate igneous rocks, are summarized as the magmatic records for the Plaeo-Tethys evolution in the context of a plate tectonic cycle. (C) 2009 Elsevier B.V. All rights reserved. |
WOS关键词 | OCEAN-CONTINENT TRANSITION ; VOLCANIC RIFTED MARGIN ; RARE-EARTH PATTERNS ; FLOOD BASALTS ; RED-SEA ; ISOTOPIC CONSTRAINTS ; EASTERN SWITZERLAND ; MELT/ROCK REACTION ; CENTRAL ATLANTIC ; PASSIVE-MARGIN |
WOS研究方向 | Geochemistry & Geophysics ; Mineralogy |
语种 | 英语 |
出版者 | ELSEVIER SCIENCE BV |
WOS记录号 | WOS:000272787200026 |
资助机构 | National Natural Science Foundation of China(40272043 ; National Natural Science Foundation of China(40272043 ; 40672048) ; 40672048) ; National Natural Science Foundation of China(40272043 ; National Natural Science Foundation of China(40272043 ; 40672048) ; 40672048) ; National Natural Science Foundation of China(40272043 ; National Natural Science Foundation of China(40272043 ; 40672048) ; 40672048) ; National Natural Science Foundation of China(40272043 ; National Natural Science Foundation of China(40272043 ; 40672048) ; 40672048) |
内容类型 | 期刊论文 |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/71767] ![]() |
专题 | 中国科学院地质与地球物理研究所 |
通讯作者 | Jian, Ping |
作者单位 | 1.Chinese Acad Geol Sci, SHRIMP Ctr, Inst Geol, Beijing 100037, Peoples R China 2.Johannes Gutenberg Univ Mainz, Inst Geowissensch, D-55099 Mainz, Germany 3.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China 4.Reg Geol Survey Yunnan Prov, Yuxi 653100, Peoples R China 5.Jilin Univ, Fac Appl Technol, Changchun 130022, Peoples R China |
推荐引用方式 GB/T 7714 | Jian, Ping,Liu, Dunyi,Kroener, Alfred,et al. Devonian to Permian plate tectonic cycle of the Paleo-Tethys Orogen in southwest China (I): Geochemistry of ophiolites, arc/back-arc assemblages and within-plate igneous rocks[J]. LITHOS,2009,113(3-4):748-766. |
APA | Jian, Ping.,Liu, Dunyi.,Kroener, Alfred.,Zhang, Qi.,Wang, Yizhao.,...&Zhang, Wei.(2009).Devonian to Permian plate tectonic cycle of the Paleo-Tethys Orogen in southwest China (I): Geochemistry of ophiolites, arc/back-arc assemblages and within-plate igneous rocks.LITHOS,113(3-4),748-766. |
MLA | Jian, Ping,et al."Devonian to Permian plate tectonic cycle of the Paleo-Tethys Orogen in southwest China (I): Geochemistry of ophiolites, arc/back-arc assemblages and within-plate igneous rocks".LITHOS 113.3-4(2009):748-766. |
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