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桂西隆林-西林地区辉绿岩成因:峨眉山地幔柱外带岩浆作用的启示

邓发亮 姚野 刘希军 李政林 张付胜 时毓 付伟 廖帅

桂林理工大学学报2017,Vol.37Issue(2):231-244,14.
桂林理工大学学报2017,Vol.37Issue(2):231-244,14.DOI:10.3969/j.issn.1674-9057.2017.02.001

桂西隆林-西林地区辉绿岩成因:峨眉山地幔柱外带岩浆作用的启示

Origin of mafic dykes from Longlin-Xilin in western Guangxi:implication for periphery magmatism of the Emeishan mantle plume

邓发亮 1姚野 2刘希军 3李政林 3张付胜 3时毓 3付伟 3廖帅3

作者信息

  • 1. 桂林理工大学广西有色金属隐伏矿床勘查及材料开发协同创新中心,广西桂林541004
  • 2. 桂林理工大学广西隐伏金属矿产勘查重点实验室,广西桂林541004
  • 折叠

摘要

Abstract

The layered intruded mafic lavas and dikes are well cropped out around the Longlin-Xilin area in western Guangxi.The petrogenesis study of the mafic dikes will better understand the tectonic-magmatic significance of this region.Petrographic and major trace element geochemical data show that the mafic dikes belong to alkaline basalt with low SiO2and high TiO2,MgO,LREE-enriched characteristics,with Ti/Y =579-742,(La/Yb) N =6.70--10.20,Nb/U =23-33 and Nb/La =0.80-0.94.Thus,the geochemical features of dikes akin to the Emeishan large igneous province(ELIP) high-Ti basalts,but they possess the slightly depleted Zr,Hf and Y,and indicate such a melt from the partial melting plume mantle source when experiencing the weak crustal contamination.The low (87Sr/86Sr)t(from 0.705 023 to 0.705 782) and high eNd(from +0.7 to + 1.0),akin to ELIP high-Ti basalts and other high-Ti mafic rocks of western Guangxi,suggest that the Longlin-Xilin mafic dikes most likely represent a part of outer zone of the ELIP plume magmatism.From the regional tectonic relationships between the mafic dikes and the fine-disseminated gold deposits as well as the extensive evolved carbonate platform uplifting,we further conclude that the ore-forming process of gold deposit resembles to that of Nevada's Carlin-type gold deposit in US,the interaction between the Emeishan plume and Paleotethyan subduction zone induced the regional gold deposits.

关键词

基性岩/地幔柱/微细浸染型金矿/隆林-西林地区

Key words

mafic dykes/mantle plumb/fine-disseminated gold deposit/Longlin-Xilin area

分类

天文与地球科学

引用本文复制引用

邓发亮,姚野,刘希军,李政林,张付胜,时毓,付伟,廖帅..桂西隆林-西林地区辉绿岩成因:峨眉山地幔柱外带岩浆作用的启示[J].桂林理工大学学报,2017,37(2):231-244,14.

基金项目

国家自然科学基金项目(41463002) (41463002)

广西科学研究与技术开发计划项目(桂科能1598025-14) (桂科能1598025-14)

广西自然科学基金项目(2014GXNSFBA118218 ()

2014GXNSFBA11820) ()

同位素地球化学国家重点实验室(中国科学院广州地球化学研究所)开放基金项目(AKLIG-KF-14-04) (中国科学院广州地球化学研究所)

广西“八桂学者”创新团队项目(2013,有色金属成矿理论与勘查技术) (2013,有色金属成矿理论与勘查技术)

桂林理工大学学报

OA北大核心CSTPCD

1674-9057

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