| 江西邓家山地区构造特征与找矿有利部位分析 |
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| 引用本文： | 龙昱,曹钟清,余忠珍. 江西邓家山地区构造特征与找矿有利部位分析[J]. 江西地质, 1997, 0(2) |
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| 作者姓名： | 龙昱 曹钟清 余忠珍 |
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| 作者单位： | 中国地质大学，江西地质矿产勘查开发局赣西北地质大队 |
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| 摘 要： | 本文根据邓家山地区构造分区、分段和空间形态与结构的研究，得出该区的地质构造主要是多期自南向北挤压作用的结果，并受到后期岩浆侵入作用的影响。在此基础上分析得出，有利的成矿地段和成矿构造部位与隐伏岩体、矿体的埋深向南逐渐加深的结论。
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| 关 键 词： | 背斜 逆冲断层 岩体 矿体 矿化裂隙 邓家山地区 |
AN ANALYSIS ON STRUCTURAL FEATURES AND ORE POTENTIAL LOCATIONS IN THEDENGJIASHAN AREA,JIANGXI |
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| Long Yu ,Cao Zhongqing and Yu Zhongzhen. AN ANALYSIS ON STRUCTURAL FEATURES AND ORE POTENTIAL LOCATIONS IN THEDENGJIASHAN AREA,JIANGXI[J]. Jiangxi Geology, 1997, 0(2) |
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| Authors: | Long Yu Cao Zhongqing Yu Zhongzhen |
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| Affiliation: | Long Yu 1,Cao Zhongqing 2 and Yu Zhongzhen 2 |
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| Abstract: | Based on study of the spacial forms and structures in subdistricts and subsections of the Dengjiashan area,this paper comes to a conclusion that the geological structures in this area were formed mainly by multistage comperssion from south to north and were subsequently influenced by post-magmatic intrusion. On this basis another conclusion may also be drawn that the ore potential locations , the orecontrolling structures, the orerelated magmatic rocks and the potential ore bodies are buried deeper and deeper southward. |
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| Keywords: | anticline thrust magmatic rock body orebody mineralized fracture |
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