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胶东焦家金矿床有限应变分析及其意义
引用本文:丁式江,翟裕生,邓军. 胶东焦家金矿床有限应变分析及其意义[J]. 地质找矿论丛, 1997, 12(4): 9-16
作者姓名:丁式江  翟裕生  邓军
作者单位:中国地质大学!北京,100083
摘    要:焦家金矿床构造岩中广泛发育变形石英颗粒,这些变形石英颗粒的三维有限应变分析表明,金矿定位于断裂带的扩容空间中,会林参数普遍表现为拉伸型,体积应变为增中型,金矿体就位于强应变与相对弱应变的转换部位,构造央垢有限应变椭球体拉伸轴主要中于NE-SW向,含矿热液运移方向与焦家断裂带平行,成矿过程中体系是开放的,有大量体系外物质迁入。

关 键 词:断裂带 有限应变分析 金矿床 矿床地质
收稿时间:1997-08-04
修稿时间:1997-08-25

STRAIN ANALYSIS AND ITS IMPLICATION FOR JIAOJIA GOLD DEPOSIT IN EASTERN SHANDONG
Ding Shijiang,Zhai Yushen and Deng Jun. STRAIN ANALYSIS AND ITS IMPLICATION FOR JIAOJIA GOLD DEPOSIT IN EASTERN SHANDONG[J]. Contributions to Geology and Mineral Resources Research, 1997, 12(4): 9-16
Authors:Ding Shijiang  Zhai Yushen  Deng Jun
Affiliation:China University of Geosciences, Beijing, 100083;China University of Geosciences, Beijing, 100083;China University of Geosciences, Beijing, 100083
Abstract:Jiaojia fault is a very important gold mineralization zone in Eastern Shandong. Deformedquartz is widely developed in Jiaojia gold deposit. Three-dimension strain analysis of the quartzgrains indicates that gold deposit is located in dilation space of the fault zone, Flinn parametersare usually extension style, volume strains are raised. Gold ore is located in transfer sites betweenstrong and weak strain. The extensional axises of strain ellipsoid are mainly NE-SW direction.The ore fluid immigrates along Jiaojia fault zone. The ore-forming system is open and lots of materials are immigrated into the system during the mineralization.
Keywords:Jiaojia fault zone strain analysis gold deposit
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