Origin of early Cretaceous calc-alkaline lamprophyres from the Sulu orogen in eastern China: implications for enrichment processes beneath continental collisional belt | |
Guo, F ; Fan, WM ; Wang, YJ ; Zhang, M | |
刊名 | LITHOS
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2004 | |
卷号 | 78期号:3页码:291-305 |
关键词 | geochemistry lamprophyres early cretaceous mantle metasomatism continental subduction The Sulu orogen |
ISSN号 | 0024-4937 |
通讯作者 | guofengt@263.net |
中文摘要 | K-Ar dating, major- and trace-element and Sr-Nd isotopic analyses were carried out for early Cretaceous (122-127 Ma) lamprophyres from the Sulu orogen in eastern China. The results show strong fractionation in rare-earth elements with (LREE) >100 times chondrite, but HREE < 10 times chondrite, indicating the presence of residual garnet in the melting source. These rocks are characterized by significant LILE and LREE enrichment but Nb and Ta depletion with moderate Zr/Hf (39.8-50.8 with regard to 36 for primitive mantle) and Nb/Ta (17.8-23.0, compared with 17.5 for primitive mantle) fractionations, probably as a consequence of carbonate- and rutile-rich melt metasomatism induced by dehydration and/or melting of subducted continental slab at mantle depths. Age-correlated Sr-Nd isotope ratios show moderate ranges of Sr-87/Sr-86(i) from 0.70787 to 0.70934 and - 17.2 to - 11.6 Of epsilon(Nd)(t). The lamprophyres from the Sulu orogen were derived from decompression melting of such a metasomatized lithospheric mantle that was mainly composed of phlogophite garnet peridotites and experienced crystal fractionation of a mineral assemblage of olivine +/- clinopyroxene plagioclase en route to the Surface. Such geochemical and isotopic signatures are also prevalent in the contemporaneous basaltic lavas in the Dabie-Sulu belt, suggesting predominant enrichment processes by carbonate- and rutile-rich metasomatic assemblage beneath the continental collisional belt. (C) 2004 Elsevier B.V. All rights reserved. |
学科主题 | Geochemistry & Geophysics; Mineralogy |
收录类别 | SCI |
原文出处 | ELSEVIER SCIENCE BV |
WOS记录号 | WOS:000224610300003 |
公开日期 | 2011-07-03 |
内容类型 | 期刊论文 |
源URL | [http://ir.scsio.ac.cn/handle/344004/4778] ![]() |
专题 | 南海海洋研究所_中科院边缘海地质重点实验室 |
推荐引用方式 GB/T 7714 | Guo, F,Fan, WM,Wang, YJ,et al. Origin of early Cretaceous calc-alkaline lamprophyres from the Sulu orogen in eastern China: implications for enrichment processes beneath continental collisional belt[J]. LITHOS,2004,78(3):291-305. |
APA | Guo, F,Fan, WM,Wang, YJ,&Zhang, M.(2004).Origin of early Cretaceous calc-alkaline lamprophyres from the Sulu orogen in eastern China: implications for enrichment processes beneath continental collisional belt.LITHOS,78(3),291-305. |
MLA | Guo, F,et al."Origin of early Cretaceous calc-alkaline lamprophyres from the Sulu orogen in eastern China: implications for enrichment processes beneath continental collisional belt".LITHOS 78.3(2004):291-305. |
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