Tracing a subducted ridge-transform system in a late Carboniferous accretionary prism of the southern Altaids: Orthogonal sanukitoid dyke swarms in Western Junggar, NW China
文献类型：期刊论文
| 作者 | Ma, Chong1,2,3; Xiao, Wenjiao1,3; Windley, Brian F.4; Zhao, Guiping2; Han, Chunming1,3; Zhang, Ji'en1,3; Luo, Jun1,3; Li, Chao1,3 |
| 刊名 | LITHOS
 |
| 出版日期 | 2012-05-01 |
| 卷号 | 140页码:152-165 |
| 关键词 | Dyke swarms Sanukitoids Paleostress inversion Ridge subduction Western Junggar Altaids |
| ISSN号 | 0024-4937 |
| DOI | 10.1016/j.lithos.2012.02.005 |
| 文献子类 | Article |
| 英文摘要 | Two sets of Late Paleozoic, orthogonal, dioritic dyke swarms are defined in the eastern part of the Western Junggar accretionary collage in the southern Altaids. Dioritic dykes (hornblende + plagioclase) are characterized by relatively high SiO2, elevated MgO, Na2O, K2O, Mg-#, Ni, Si and Cr contents, La/Yb ratios, very low Y contents, and enrichments in large ion lithophile elements (LILE) and light rare earth elements (LREE), which are all comparable with those of sanukitoids. These dioritic dykes have low (Sr-87/Sr-86) ratios (mostly between 0.70366 and 0.70381) and high positive epsilon(Nd) (t) (+6.6 to +8.4) values, suggesting they were sourced from a depleted mantle. Accordingly, these dioritic dykes were probably derived by mixing of depleted mantle components that originated from upwelling of asthenosphere through a slab window with melts that were derived by dehydration of a subducted slab. Detailed mapping and structural data of the dyke swarms indicate that the NW/SE-trending set was earlier than the NE/SW-trending dykes. Paleostress analysis and inversion of the dyke swarms indicate that an early NE/SW-extension was associated with a NW/SE-trending slab window, and was followed by a slightly later NW/SE-extension that was associated with a NE/SW-trending slab window. Field relationships, together with published age constraints, suggest that these two dyke swarms were intruded in the Late Carboniferous. Therefore two orthogonal slab windows were opened, one (NE-SW) after the other (NW-SE) during this time period. A subducted ridge transform system could well account for, and is consistent with, these relationships. We propose that in the Late Carboniferous a NW/SE-trending mid-oceanic ridge was subducted beneath the Darbut trench generating large-scale, closely spaced NW/SE-trending dykes that were intruded through a slab window. That event was followed by subduction of a NE/SW-trending transform fault (fracture zone) that connected with the earlier NW/SE-trending ridge, producing widely spaced NE/SW-trending dykes that were intruded through a NE/SW-trending vertical slab window. This new approach to the relationships between dyke swarms, adakitic/sanukitoid magmatism, ridge subduction and slab windows has broad implications for tectonic reconstruction of ancient accretionary orogens. (C) 2012 Elsevier B.V. All rights reserved. |
| WOS关键词 | SETOUCHI VOLCANIC BELT ; HIGH-MAGNESIAN ANDESITES ; LOWER CONTINENTAL-CRUST ; HIGH-MG DIORITES ; CENTRAL-ASIA ; SLAB WINDOW ; TECTONIC EVOLUTION ; SOUTHWEST JAPAN ; NORTH-AMERICA ; PALEOSTRESS RECONSTRUCTIONS |
| WOS研究方向 | Geochemistry & Geophysics ; Mineralogy |
| 语种 | 英语 |
| WOS记录号 | WOS:000303095400011 |
| 出版者 | ELSEVIER SCIENCE BV |
| 资助机构 | Major State Basic Research Development Program of China(2007CB411307) ; Major State Basic Research Development Program of China(2007CB411307) ; Chinese Academy of Sciences(KZCX2-YW-Q04-08) ; Chinese Academy of Sciences(KZCX2-YW-Q04-08) ; National Natural Science Foundation of China(40725009 ; National Natural Science Foundation of China(40725009 ; 40772136) ; 40772136) ; Major State Basic Research Development Program of China(2007CB411307) ; Major State Basic Research Development Program of China(2007CB411307) ; Chinese Academy of Sciences(KZCX2-YW-Q04-08) ; Chinese Academy of Sciences(KZCX2-YW-Q04-08) ; National Natural Science Foundation of China(40725009 ; National Natural Science Foundation of China(40725009 ; 40772136) ; 40772136) ; Major State Basic Research Development Program of China(2007CB411307) ; Major State Basic Research Development Program of China(2007CB411307) ; Chinese Academy of Sciences(KZCX2-YW-Q04-08) ; Chinese Academy of Sciences(KZCX2-YW-Q04-08) ; National Natural Science Foundation of China(40725009 ; National Natural Science Foundation of China(40725009 ; 40772136) ; 40772136) ; Major State Basic Research Development Program of China(2007CB411307) ; Major State Basic Research Development Program of China(2007CB411307) ; Chinese Academy of Sciences(KZCX2-YW-Q04-08) ; Chinese Academy of Sciences(KZCX2-YW-Q04-08) ; National Natural Science Foundation of China(40725009 ; National Natural Science Foundation of China(40725009 ; 40772136) ; 40772136) |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/84554]  |
| 专题 | 中国科学院地质与地球物理研究所 |
| 通讯作者 | Xiao, Wenjiao |
| 作者单位 | 1.Chinese Acad Sci, State Key Lab Lithospher Evolut, Inst Geol & Geophys, Beijing 100029, Peoples R China 2.Chinese Acad Sci, Grad Univ, Coll Earth Sci, Lab Computat Geodynam, Beijing 100049, Peoples R China 3.Chinese Acad Sci, Xinjiang Res Ctr Mineral Resources, Xinjiang Inst Ecol & Geog, Urumqi 830011, Peoples R China 4.Univ Leicester, Dept Geol, Leicester LE1 7RH, Leics, England |
| 推荐引用方式 GB/T 7714 | Ma, Chong,Xiao, Wenjiao,Windley, Brian F.,et al. Tracing a subducted ridge-transform system in a late Carboniferous accretionary prism of the southern Altaids: Orthogonal sanukitoid dyke swarms in Western Junggar, NW China[J]. LITHOS,2012,140:152-165. |
| APA | Ma, Chong.,Xiao, Wenjiao.,Windley, Brian F..,Zhao, Guiping.,Han, Chunming.,...&Li, Chao.(2012).Tracing a subducted ridge-transform system in a late Carboniferous accretionary prism of the southern Altaids: Orthogonal sanukitoid dyke swarms in Western Junggar, NW China.LITHOS,140,152-165. |
| MLA | Ma, Chong,et al."Tracing a subducted ridge-transform system in a late Carboniferous accretionary prism of the southern Altaids: Orthogonal sanukitoid dyke swarms in Western Junggar, NW China".LITHOS 140(2012):152-165. |
入库方式： OAI收割
来源：地质与地球物理研究所
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