[1]余研.1992.地洼激烈期金推城-栾川钼矿带斑岩建造特征及其构造背景.大地构造与成矿学,16(2):146-146.
 YU Yan.1992.CHARACTERISTICS AND TECTONIC BACKGROUND OF DIWA PORPHYRITIC FORMATION IN JINDUICHENG-LUANCHUAN MOLYBDENUM DEPOSIT ZONE.Geotectonica et Metallogenia,16(2):146-146.
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地洼激烈期金推城-栾川钼矿带斑岩建造特征及其构造背景
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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:
146-146
栏目:
出版日期:
1992-05-15

文章信息/Info

Title:
CHARACTERISTICS AND TECTONIC BACKGROUND OF DIWA PORPHYRITIC FORMATION IN JINDUICHENG-LUANCHUAN MOLYBDENUM DEPOSIT ZONE
作者:
余研;
武汉化工学院 湖北武汉 430073;
Author(s):
YU Yan
Wuhan College of Chemical Technology, Wuhan, Hubei, 430073
关键词:
华北 构造背景 建造特征 成矿作用 地洼区 钾长花岗斑岩 铜矿床 深大断裂 栾川 斑岩钼矿
摘要:
华北地洼区南缘在J2-K进入激烈期,强烈的构造、岩浆及其成矿作用在唐家沟断裂以南、灵口-庙子断裂以北,形成金堆城-栾川斑岩钼矿带。斑岩及其铜矿床沿EW-NWW向,与深大断裂系平行,星长200km带状展布;沿NE-NEE向,与地洼新生次级断裂系平行,构成亚带。

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更新日期/Last Update: 2011-04-29