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湘南荷花坪锡铅锌矿区燕山期黑云母花岗岩的厘定

章荣清 陆建军 王汝成 姚远 朱金初 马东升

高校地质学报2011,Vol.17Issue(4):513-520,8.
高校地质学报2011,Vol.17Issue(4):513-520,8.

湘南荷花坪锡铅锌矿区燕山期黑云母花岗岩的厘定

The Confirmation of Yanshanian Biotite Granite in the Hehuaping Sn-Pb-Zn District, Southern Hunan Province, China

章荣清 1陆建军 1王汝成 1姚远 1朱金初 1马东升1

作者信息

  • 1. 内生金属矿床成矿研究国家重点实验室,南京大学地球科学与工程学院,南京210093
  • 折叠

摘要

Abstract

The Wangxianling granite was emplaced at the Indosinian (Triassic) period. The previous research considered that the Hehuaping Sn-Pb-Zn deposit was an Indosinian deposit related to the Wangxianling pluton. Based on many years of investigation in the field and study of rocks from drilling holes, a buried pluton with lithological characteristics different from the Wangxianling granite was discovered in the Hehuaping district. A zircon U-Pb age of (157.1 ± 0.8) Ma for the coarse-grained biotite granite from drilling hole was obtained by La-MC-ICP-MS, which suggests an early Yanshanian (Jurassic) emplacement. This granite is characterised by A/CNK value of 1.02, total REE content of 357 x 10"*, LREE/HREE ratio of 2.83 and Zr+Nb+Ce+Y content of 398 x 10-6, on average. These features are similar to those of A-type granite and markedly different from those of the Wangxianling S-type granite. This Yanshanian granite, named as Hehuaping granite, has an affinity of the tin-bearing granites in the Nanling Range. Therefore, we argue that the Hehuaping Sn-Pb-Zn deposit is related to the Yanshanian buried Hehuaping pluton.

关键词

锆石U-Pb年龄/黑云母花岗岩/荷花坪锡铅锌矿

Key words

zircon U-Pb geochronology/biotite granite/Hehuaping Sn-Pb-Zn mine

分类

天文与地球科学

引用本文复制引用

章荣清,陆建军,王汝成,姚远,朱金初,马东升..湘南荷花坪锡铅锌矿区燕山期黑云母花岗岩的厘定[J].高校地质学报,2011,17(4):513-520,8.

基金项目

中国地质调查局调查项目"南岭重要金属矿床成矿机理研究和找矿潜力预测"(1212010632100) (1212010632100)

国家自然科学基金(40730423,40873029) (40730423,40873029)

"深部探测技术与实验研究专项"(Sino Probe-03-01-4D)联合资助 (Sino Probe-03-01-4D)

高校地质学报

OA北大核心CSCDCSTPCD

1006-7493

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