Geochemistry of the chaokeshan ophiolite: product of intra-oceanic back-arc basin? | |
Wang ShuQing1,2; Xu JiFeng1; Liu XiJun1,2; Hou QingYe3 | |
刊名 | Acta petrologica sinica |
2008-12-01 | |
卷号 | 24期号:12页码:2869-2879 |
关键词 | Ophiolite Geochemistry Back-arc basin Intra-oceanic arc Chaokeshan Inner mongolia |
ISSN号 | 1000-0569 |
通讯作者 | Wang shuqing() |
英文摘要 | Chaokeshan ophiolite, one of the best-outcropped ophiolitic blocks in inner mongolia region, likely formed in late carboniferous. the chondrite-normalized ree patterns of the mafic rocks of the chaokeshan ophiolite are of characteristics of lree depletion, similar to n-morb, while the spider diagram shows the enrichment of the large iron lithosphile elements and depletion of high field strength elements-the unique feature of the are volcanic rocks, so the tectonic setting of chaokeshan ophiolite may be back-arc basin. compared with modem intra-oceanic arc mariana trough basalts, continental marginal are okinawa trough hasalts and mafic rocks of the kuerti ophiolite which formed in paleo-intra-oceanic back-arc basin, the chaokeshan mafic rocks show geochemical characteristics similar to mariana and kuerti basalts, we suggest that the chaokeshan ophiolite was likely produced in an intra-oceanic back-are tectonic setting instead of continental margin back-arc basin. |
WOS关键词 | RARE-EARTH-ELEMENTS ; ASIAN OROGENIC BELT ; INNER-MONGOLIA ; HEGENSHAN OPHIOLITE ; TECTONIC EVOLUTION ; NORTHEAST CHINA ; INDIAN-OCEAN ; MANTLE ; MORB ; PETROGENESIS |
WOS研究方向 | Geology |
WOS类目 | Geology |
语种 | 英语 |
出版者 | SCIENCE PRESS |
WOS记录号 | WOS:000262521400021 |
内容类型 | 期刊论文 |
URI标识 | http://www.corc.org.cn/handle/1471x/2386250 |
专题 | 中国科学院大学 |
通讯作者 | Wang ShuQing |
作者单位 | 1.Chinese Acad Sci, Key Lab Isotope Geochronol & Geochem, Guangzhou Inst Geochem, Guangzhou 510640, Peoples R China 2.Chinese Acad Sci, Grad Univ, Beijing 100039, Peoples R China 3.China Univ Geosci, Sch Earth Sci & Resources, Beijing 100083, Peoples R China |
推荐引用方式 GB/T 7714 | Wang ShuQing,Xu JiFeng,Liu XiJun,et al. Geochemistry of the chaokeshan ophiolite: product of intra-oceanic back-arc basin?[J]. Acta petrologica sinica,2008,24(12):2869-2879. |
APA | Wang ShuQing,Xu JiFeng,Liu XiJun,&Hou QingYe.(2008).Geochemistry of the chaokeshan ophiolite: product of intra-oceanic back-arc basin?.Acta petrologica sinica,24(12),2869-2879. |
MLA | Wang ShuQing,et al."Geochemistry of the chaokeshan ophiolite: product of intra-oceanic back-arc basin?".Acta petrologica sinica 24.12(2008):2869-2879. |
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