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DOI | 10.1016/j.epsl.2006.11.019 |
Postcollisional calc-alkaline lavas and xenoliths from the southern Qiangtang terrane, central Tibet | |
Ding, Lin; Kapp, Paul; Yue, Yahui; Lai, Qingzhou | |
发表日期 | 2007 |
ISSN | 0012-821X |
EISSN | 1385-013X |
起始页码 | 28 |
结束页码 | 38 |
卷号 | 254期号:1-2 |
英文摘要 | A newly recognized east-west trending province of 43 to 28 Ma volcanic rocks occurs in the southern Qiangtang terrane of central Tibet. The lavas are Na-rich calc-alkaline in composition, relatively primitive, and locally host ultramafic and mafic xenoliths. Foliated mafic granulite xenoliths from similar to 28 Ma lavas equilibrated at temperatures in the range of 980 to 1260 degrees C, indicating that the southern Qiangtang terrane lower crust was deformed and heated to very high temperatures during or before the Oligocene. In the northern Qiangtang terrane is a parallel suite of volcanic rocks of coeval age. However, here, the volcanic rocks are (ultra)potassic in composition and underlain by a hot (T > 800 degrees C) metasedimentary-bearing lower crust. We suggest that both suites of Qiangtang lavas were derived from a primitive mantle source and that the enriched nature of the northern Qiangtang lavas reflects contamination by partial melts of metasedimentary lower crust. This contrasts with the conventional interpretation that Tibetan potassic lavas were solely derived from an ancient, enriched mantle lithospheric source. While removal of lithospheric mantle seems to be required to produce the high temperature melts, Eocene-Oligocene volcanism was coeval with thrust reactivation along bounding suture zones, implying that mantle dynamics were linked to intracontinental subduction. (c) 2006 Elsevier B.V. All rights reserved. |
关键词 | EAST-WEST EXTENSIONNORTHERN TIBETTECTONIC EVOLUTIONCRUSTAL XENOLITHSVOLCANIC-ROCKSPLATEAUUPLIFTMAGMATISMCOLLISIONLHASA |
英文关键词 | Tibetan plateau; postcollisional volcanism; xenoliths; intracontinental subduction |
语种 | 英语 |
WOS研究方向 | Geochemistry & Geophysics |
WOS类目 | Geochemistry & Geophysics |
WOS记录号 | WOS:000244595000003 |
来源期刊 | EARTH AND PLANETARY SCIENCE LETTERS |
来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/257477 |
推荐引用方式 GB/T 7714 | Ding, Lin,Kapp, Paul,Yue, Yahui,et al. Postcollisional calc-alkaline lavas and xenoliths from the southern Qiangtang terrane, central Tibet[J]. 中国科学院青藏高原研究所,2007,254(1-2). |
APA | Ding, Lin,Kapp, Paul,Yue, Yahui,&Lai, Qingzhou.(2007).Postcollisional calc-alkaline lavas and xenoliths from the southern Qiangtang terrane, central Tibet.EARTH AND PLANETARY SCIENCE LETTERS,254(1-2). |
MLA | Ding, Lin,et al."Postcollisional calc-alkaline lavas and xenoliths from the southern Qiangtang terrane, central Tibet".EARTH AND PLANETARY SCIENCE LETTERS 254.1-2(2007). |
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