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中国地质学会

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陕西太白庙金矿赵大沟矿段地质特征及构造控矿规律

邢宪龙, 王嘉伟, 胡仰军

邢宪龙, 王嘉伟, 胡仰军. 陕西太白庙金矿赵大沟矿段地质特征及构造控矿规律[J]. 西北地质, 2013, 46(2): 87-92.
引用本文: 邢宪龙, 王嘉伟, 胡仰军. 陕西太白庙金矿赵大沟矿段地质特征及构造控矿规律[J]. 西北地质, 2013, 46(2): 87-92.
XING Xian-long, WANG Jia-wei, HU Yang-jun. Deep Structures and Their Constraints on Gold Mineralization in the Zhaodagou Section of the Taibaimiao Gold-ore Area Southern Shaanxi Province[J]. Northwestern Geology, 2013, 46(2): 87-92.
Citation: XING Xian-long, WANG Jia-wei, HU Yang-jun. Deep Structures and Their Constraints on Gold Mineralization in the Zhaodagou Section of the Taibaimiao Gold-ore Area Southern Shaanxi Province[J]. Northwestern Geology, 2013, 46(2): 87-92.

陕西太白庙金矿赵大沟矿段地质特征及构造控矿规律

Deep Structures and Their Constraints on Gold Mineralization in the Zhaodagou Section of the Taibaimiao Gold-ore Area Southern Shaanxi Province

  • 摘要: 赵大沟矿段各矿体的产出与分布严格受北西西向压扭性断裂(F1~F5)控制。成矿作用早期形成的张性构造裂隙是矿体的主要赋存空间,无论矿体还是张性裂隙均在深部显示为沿北西西向压扭性断裂断续延伸的规律,反映了在北西西向压扭性(F1~F5)断裂所经过矿段的深部还有延续。因此,赵大沟矿段构造控矿标志明显,预测与其相邻的赵大沟以西地区和金洞沟地区地表及深部具有相似的赋矿规律和找矿标志,应作为今后主要的找矿远景区。
    Abstract: The output and distribution of ore bodies in Zhaodagou ore section are strictly controlled by the NWW-direction F1~F5 compressive-shear fault. The tensile fracture formed in early ore-forming stage is the main accumulating space of ore body. Regardless of the ore body or tensile fracture, both of them in deep area show the intermittent extension along the F1~F5 fracture, reflecting that there is extension in the deep area of ore section that F1~F5 fracture passes through. Therefore, the structural ore-control sign of Zhaodagou ore section is clear, and it is predicated that it has the similar ore-accumulating rules and prospecting sign in ground surface and deep area with the neighboring western area of Zhaodagou and Jindonggou area, which can be regarded as the main prospective area to look for ore body.
  • 张国伟,张本仁,袁学诚.秦岭造山带与大陆动力学[M].北京:科学出版社,2001:501-508.

    Zhang Guowei,Zhang Benren,Yuan Xuecheng,Qinling Orogenic Beit and Continental Dynamus[M].Science Press, Beijing,2001,501-508.

    陕西区调队. 陕西区域地质志[M].北京:地质出版社,1989:528-530.

    Shaanxi Institute of Regional Survey. Regional Geology of Shaanxi Province,Peoples Republic of Chuia[M].Geologic Publishing House,Beijing,1989,528-530.

    陕西区调队. 陕西省镇安—柞水地区1:5万区域地质调查报告.1996:145-182.

    宗静婷.陕西略阳铧厂沟金矿床地质特征与矿床类型[J].西北地质,2004,37(1):97-101.

    Zong Jingting.Features of Huachanggou gold deposit and its type in Lueyang county,Shaaxi[J].Northwestern Geology,2004,37(1):97-101.

    马中平,魏宽义.陕西镇安五岭微细浸染型金矿床金矿化过程中元素活动规律[J].西北地质,2005,38(1):73-77.

    Ma Zhongping,Wei Kuanyi. Regularities of element activities in golod-mineralizing process of the Qiuling miero-disseminated gold deposits in Zhen'an,Shannxi[J].Northwestern Geology,2005,38(1):73-77.

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出版历程
  • 收稿日期:  2012-08-30
  • 修回日期:  2013-02-19
  • 发布日期:  2013-06-04

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