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印尼苏门答腊岛苏利特河铜矿地质特征

向文帅 高小卫 程湘

华南地质与矿产Issue(4):361-367,7.
华南地质与矿产Issue(4):361-367,7.DOI:10.3969/j.issn.1007-3701.2014.04.007

印尼苏门答腊岛苏利特河铜矿地质特征

Geological characteristics of Sulit Air Copper deposit in Suma-tra Indonesia

向文帅 1高小卫 1程湘1

作者信息

  • 1. 中国地质调查局武汉地质调查中心,武汉 430205
  • 折叠

摘要

Abstract

Sulit Air copper deposit belongs to the Jurassic- early Cretaceous magma arc related copper-gold metallogenic period of Sumatra, Indonesia. In order to summarize the characteristics of this deposit and to guide the prospecting in this area, this article study the geology, petrology and geochemistry of Sulit Air. Geochemistry characteristic shows that the skarn rocks have more CaO and less Al2O3, K2O, Na2O content than the igneous rock;In the FAM diagram and FeOt-MgO-Al2O3 diagram, the skarn rock dropped near the igneous rocks area. Howev-er, the REE pattern of those two rocks are different, the Σw (REE) of igneous rock is higher than skarn rock; the skarn rocks have negative europium anomalies rather than positive anomalies in the igneous rock. In conclusion, the age of Sulit Air deposit is later than early-Jurassic and its ore-forming setting belongs to the post-orogenic and post-collisional volcanism.

关键词

苏利特河铜矿/矽卡岩/稀土元素/苏门答腊岛

Key words

Sulit Air copper deposit/geochemistry/skarn/Sumatra

分类

天文与地球科学

引用本文复制引用

向文帅,高小卫,程湘..印尼苏门答腊岛苏利特河铜矿地质特征[J].华南地质与矿产,2014,(4):361-367,7.

基金项目

中国地质调查局项目“印度尼西亚中苏门答腊岛铜、金等多金属矿产成矿规律研究(1212011120339)” ()

华南地质与矿产

1007-3701

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