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
DOI10.1016/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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