[1]陈文明.1992.我国地洼型斑岩、矽卡岩铜、钼矿床的地质特征及形成机制.大地构造与成矿学,16(2):145-145.
 CHEN Wenming.1992.GEOLOGICAL CHARACTERISTICS AND FORMATION MECHANISM OF PORPHYRY AND SKARN Cu-Mo DEPOSITS OF DIWA TYPE IN CHINA.Geotectonica et Metallogenia,16(2):145-145.
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我国地洼型斑岩、矽卡岩铜、钼矿床的地质特征及形成机制
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《大地构造与成矿学》[ISSN:ISSN 1001-1552/CN:CN 44-1595/P]

卷:
期数:
1992年16卷02期
页码:
145-145
栏目:
出版日期:
1992-05-15

文章信息/Info

Title:
GEOLOGICAL CHARACTERISTICS AND FORMATION MECHANISM OF PORPHYRY AND SKARN Cu-Mo DEPOSITS OF DIWA TYPE IN CHINA
作者:
陈文明;
中国地质科学院矿床地质研究所 北京 100037;
Author(s):
CHEN Wenming
Institute of Mineral Deposits, Chinese Academy of Geological Science,Beijing, 100037
关键词:
地洼型 白云岩 矽卡岩型铜矿 地质特征 形成机制 钼矿床 斑岩体 地层时代 中酸性岩体 地洼区
摘要:
据我国已有的120个斑岩、矽卡岩型Cu-Mo矿床的资料,我国有84.7%的斑岩、矽卡岩型铜矿和96.5%的斑岩、矽卡岩型钼矿位于地洼区,并形成于地洼阶段,属地洼型矿床。该类矿床与形成于地槽阶段的斑岩、矽卡岩型Cu-Mo矿床相比具以下特征: 1、与该类Cu-Mo矿床伴生的中酸性岩体一般形成于燕山-喜山期,其形成的时代与其赋存围岩地层时代相距较远,岩体规模较

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更新日期/Last Update: 2011-04-29