Magmatic and metamorphic development of an early to mid-Paleozoic;continental margin arc in the southernmost Central Asian Orogenic Belt,;Inner Mongolia, China | |
Zhang, Wei3; Jian, Ping; Kroener, Alfred1; Shi, Yuruo | |
刊名 | JOURNAL OF ASIAN EARTH SCIENCES |
2013 | |
卷号 | 72;SI SI页码:63-74 |
关键词 | Zircon Continental margin arc Magmatism Metamorphism Central Asian Orogenic Belt Paired metamorphic belts |
ISSN号 | 1367-9120;EI 1878-5786 |
DOI | 10.1016/j.jseaes.2012.05.025 |
英文摘要 | The Bainaimiao arc in Inner Mongolia, China, comprises a weakly metamorphosed volcani-sedimentary sequence and a low-P/T metamorphic complex. In this study we present SHRIMP zircon ages and geochemical data to document the temporal and genetic relationships between these two tectonic units. Zircons from a rhyolite and two dacites (high-K calc-alkaline) of the volcani-sedimentary sequence yielded Pb-206/U-238 ages of 474 +/- 7 Ma, 453 +/- 7 Ma and 436 +/- 9 Ma respectively, that we interpret as recording the timing of three volcanic arc episodes. Rocks from the low-P/T metamorphic complex yielded zircon ages of 462 +/- 11 Ma for a sillimanite gneiss and 437 +/- 5 Ma for a plagioclase-hornblende gneiss, reflecting two distinct anatectic events. Also from the low-P/T complex, the protolith age of a metadiorite is 438 +/- 2 Ma. A diorite from a weakly deformed diorite-granodiorite pluton in the low-P/T complex has a zircon age of 419 +/- 10 Ma that correlates in time with regional collisional magmatism. An undeformed pegmatite dike cutting the low-P/T metamorphic complex has an age of 411 +/- 8 Ma, which postdates collision and provides an upper limit for the termination of orogeny. Accordingly, we conclude that the volcani-sedimentary sequence and the low-P/T metamorphic complex evolved coherently in the early to mid-Paleozoic and formed an integral continental margin arc in the southernmost Central Asian Orogenic Belt. (c) 2012 Elsevier Ltd. All rights reserved. |
学科主题 | 火成岩岩石学 |
WOS关键词 | ARABIAN-NUBIAN SHIELD ; U-PB AGES ; CENTRAL AUSTRALIA ; SOLONKER SUTURE ; TIME-SCALE ; ZIRCON ; ZONE ; PETROGENESIS ; ACCRETION ; GROWTH |
WOS研究方向 | Geology |
语种 | 英语 |
出版者 | PERGAMON-ELSEVIER SCIENCE LTD |
WOS记录号 | WOS:000321404900006 |
内容类型 | 期刊论文 |
源URL | [http://119.78.100.197/handle/2HKVOGP0/40169] |
专题 | 中国地质科学院地质研究所 |
作者单位 | 1.Chinese Acad Geol Sci, Inst Geol, SHRIMP Ctr, Beijing 100037, Peoples R China. 2.Johannes Gutenberg Univ Mainz, Inst Geowissensch, D-55099 Mainz, Germany. 3.中国地质科学院地质研究所 |
推荐引用方式 GB/T 7714 | Zhang, Wei,Jian, Ping,Kroener, Alfred,et al. Magmatic and metamorphic development of an early to mid-Paleozoic;continental margin arc in the southernmost Central Asian Orogenic Belt,;Inner Mongolia, China[J]. JOURNAL OF ASIAN EARTH SCIENCES,2013,72;SI SI:63-74. |
APA | Zhang, Wei,Jian, Ping,Kroener, Alfred,&Shi, Yuruo.(2013).Magmatic and metamorphic development of an early to mid-Paleozoic;continental margin arc in the southernmost Central Asian Orogenic Belt,;Inner Mongolia, China.JOURNAL OF ASIAN EARTH SCIENCES,72;SI SI,63-74. |
MLA | Zhang, Wei,et al."Magmatic and metamorphic development of an early to mid-Paleozoic;continental margin arc in the southernmost Central Asian Orogenic Belt,;Inner Mongolia, China".JOURNAL OF ASIAN EARTH SCIENCES 72;SI SI(2013):63-74. |
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