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DOI | 10.1016/j.precamres.2014.01.009 |
Neoproterozoic subduction along the Ailaoshan zone, South China: Geochronological and geochemical evidence from amphibolite | |
Cai, Yongfeng; Wang, Yuejun; Cawood, Peter A.; Fan, Weiming; Liu, Huichuan; Xing, Xiaowan; Zhang, Yuzhi | |
通讯作者 | Wang, YJ (通讯作者) |
发表日期 | 2014 |
ISSN | 0301-9268 |
EISSN | 1872-7433 |
起始页码 | 13 |
结束页码 | 28 |
卷号 | 245 |
英文摘要 | Lenses of amphibolites occur along the Ailaoshan suture zone at the southwestern margin of the Yangtze Block, South China. Petrological, geochemical and zircon U-Pb geochronological data indicate that they are divisible into two coeval groups. Group 1, represented by the Jinping amphibolite, has mg-number of 71-76 and (La/Yb)cn ratios of 7.2-7.7, and displays a geochemical affinity to island arc volcanic rocks. Group 2 amphibolites occur at Yuanyang and are characterized by high Nb contents (14.3-18.4 ppm), resembling Nb-enriched basalts. The epsilon(Nd)(t) values for Group 1 range from -3.45 to -2.04 and for Group 2 from +4.08 to +4.39. A representative sample for Group 1 yields a U-Pb zircon age of 803 7 Ma, whereas two samples for Group 2 give U-Pb zircon ages of 813 +/- 11 Ma and 814 +/- 12 Ma. Petrogenetic analysis suggests that Group 1 originated from an orthopyroxene-rich source and Group 2 from a mantle wedge modified by slab-derived melt. In combination with other geological observations, these amphibolites are inferred to constitute part of an early Neoproterozoic (similar to 815-800 Ma) arc-back-arc basin system. The Neoproterozoic amphibolites and related rocks along the Ailaoshan zone may be the southward extension of the Neoproterozoic supra-subduction zone that developed along the western margin of the Yangtze Block. (C) 2014 Elsevier B.V. All rights reserved. |
关键词 | ZIRCON U-PBBACK-ARC BASINNORTHWESTERN YANGTZE BLOCKBIMODAL VOLCANIC-ROCKSRIVER SHEAR ZONEA-TYPE GRANITESTECTONIC EVOLUTIONCRUSTAL EVOLUTIONJIANGNAN OROGENNORTHERN MARGIN |
英文关键词 | Ailaoshan zone; Amphibolite; Zircon U-Pb dating; Petrogenesis; Neoproterozoic subduction |
语种 | 英语 |
WOS研究方向 | Geology |
WOS类目 | Geosciences, Multidisciplinary |
WOS记录号 | WOS:000335107000002 |
来源期刊 | PRECAMBRIAN RESEARCH |
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/258389 |
推荐引用方式 GB/T 7714 | Cai, Yongfeng,Wang, Yuejun,Cawood, Peter A.,et al. Neoproterozoic subduction along the Ailaoshan zone, South China: Geochronological and geochemical evidence from amphibolite[J]. 中国科学院青藏高原研究所,2014,245. |
APA | Cai, Yongfeng.,Wang, Yuejun.,Cawood, Peter A..,Fan, Weiming.,Liu, Huichuan.,...&Zhang, Yuzhi.(2014).Neoproterozoic subduction along the Ailaoshan zone, South China: Geochronological and geochemical evidence from amphibolite.PRECAMBRIAN RESEARCH,245. |
MLA | Cai, Yongfeng,et al."Neoproterozoic subduction along the Ailaoshan zone, South China: Geochronological and geochemical evidence from amphibolite".PRECAMBRIAN RESEARCH 245(2014). |
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