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Continental orogenesis from ocean subduction, continent collision/subduction, to orogen collapse, and orogen recycling: The example of the North Qaidam UHPM belt, NW China
文献类型：期刊论文
| 作者 | Song, Shuguang1; Niu, Yaoling2,3; Su, Li4; Zhang, Cong1; Zhang, Lifei1 |
| 刊名 | EARTH-SCIENCE REVIEWS
 |
| 出版日期 | 2014-02-01 |
| 卷号 | 129页码:59-84 |
| 关键词 | Continental-type UHPM belt Post-collisional magmatism Orogenesis and mountain collapse Decoupling of oceanic and continental subduction belts Orogen recycling Northern Tibetan Plateau |
| 通讯作者 | Song, SG (reprint author), Peking Univ, Sch Earth & Space Sci, MOE Key Lab Orogen Belts & Crustal Evolut, Beijing 100871, Peoples R China. |
| 英文摘要 | The North Qaidam ultra-high pressure metamorphic (UHPM) belt in the northern Tibetan Plateau records a complete history of the evolution of a continental orogen from prior seafloor subduction, to continental collision and subduction, and to the ultimate orogen collapse in the time period from the Neoproterozoic to the Paleozoic. Lithologies in this UHPM belt consist predominantly of felsicgneisses containing blocks of edogite and peridotite. The 1120-900 Ma granitic and psammitic/pelitic gneisses compose the majority of the UHPM belt and is genetically associated with the previous orogenic cycle of Grenville-age, whereas protoliths of the HUPM eclogites are of both the 850-820 Ma continental flood basalts (CFBs) and the 540-500 Ma oceanic crust (ophiolite). The early stage of quartz-stable eclogite-facies metamorphism took place at -445-473 Ma, the same age as that of the HP rocks in the North Qilian oceanic suture zone, representing the earliest subducting seafloor rocks exhumed and preserved. Coesite-bearing zircons from the metapelite and eclogite, diamond-bearing zircons from garnet peridotites constrain the UHP metamorphic age of -438-420 Ma, which represents the timing of continental subduction at depths of 100-200 km, -10-20 m.y. younger than the early stage of the (lian seafloor subduction. Therefore, deep subduction of continental crust should be the continuation of oceanic subduction that is pulled down by the sinking oceanic lithosphere or pushed down by the overriding upper plate, which is an expected and inevitable consequence for the scenario of passive continental margins. Partial melting of subducted ocean crust might occur in response to continental subduction at -435 Ma. |
| 学科主题 | Geology |
| 收录类别 | SCI |
| 语种 | 英语 |
| WOS记录号 | WOS:000331919500004 |
| 源URL | [http://ir.qdio.ac.cn/handle/337002/23805]  |
| 专题 | 海洋研究所_海洋地质与环境重点实验室 |
| 作者单位 | 1.Peking Univ, Sch Earth & Space Sci, MOE Key Lab Orogen Belts & Crustal Evolut, Beijing 100871, Peoples R China 2.Univ Durham, Dept Earth Sci, Durham DH1 3LE, England 3.Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China 4.Chinese Univ Geosci, Inst Earth Sci, Beijing 100083, Peoples R China |
| 推荐引用方式 GB/T 7714 | Song, Shuguang,Niu, Yaoling,Su, Li,et al. Continental orogenesis from ocean subduction, continent collision/subduction, to orogen collapse, and orogen recycling: The example of the North Qaidam UHPM belt, NW China[J]. EARTH-SCIENCE REVIEWS,2014,129:59-84. |
| APA | Song, Shuguang,Niu, Yaoling,Su, Li,Zhang, Cong,&Zhang, Lifei.(2014).Continental orogenesis from ocean subduction, continent collision/subduction, to orogen collapse, and orogen recycling: The example of the North Qaidam UHPM belt, NW China.EARTH-SCIENCE REVIEWS,129,59-84. |
| MLA | Song, Shuguang,et al."Continental orogenesis from ocean subduction, continent collision/subduction, to orogen collapse, and orogen recycling: The example of the North Qaidam UHPM belt, NW China".EARTH-SCIENCE REVIEWS 129(2014):59-84. |
入库方式： OAI收割
来源：海洋研究所
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