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中国地质学会

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凤-太多金属矿集区主要金属矿床成矿系列与找矿方向

王瑞廷, 王涛, 高章鉴, 陈二虎, 刘莉霞

王瑞廷, 王涛, 高章鉴, 等. 凤-太多金属矿集区主要金属矿床成矿系列与找矿方向[J]. 西北地质, 2007, 40(2): 77-84.
引用本文: 王瑞廷, 王涛, 高章鉴, 等. 凤-太多金属矿集区主要金属矿床成矿系列与找矿方向[J]. 西北地质, 2007, 40(2): 77-84.
WANG Rui-ting, WANG Tao, GAO Zhang-jian, et al. The Main Metal Deposits Metallogenic Series and Exploration Direction in Feng-Tai Ore Cluster Region, Shaanxi Province[J]. Northwestern Geology, 2007, 40(2): 77-84.
Citation: WANG Rui-ting, WANG Tao, GAO Zhang-jian, et al. The Main Metal Deposits Metallogenic Series and Exploration Direction in Feng-Tai Ore Cluster Region, Shaanxi Province[J]. Northwestern Geology, 2007, 40(2): 77-84.

凤-太多金属矿集区主要金属矿床成矿系列与找矿方向

The Main Metal Deposits Metallogenic Series and Exploration Direction in Feng-Tai Ore Cluster Region, Shaanxi Province

  • 摘要: 通过对凤-太多金属矿集区区域地质背景及地球化学、地球物理特征的综合研究,结合区内已知矿床的系统分析,把凤-太多金属矿集区主要金属矿床划分为3个成矿系列,即泥盆纪碳酸岩盐容矿的铅锌矿床成矿系列、泥盆纪沉积改造型铜矿床成矿系列和中生代与造山作用有关的金矿床成矿系列。提出长沟-洞沟地区、凤州七里坪地区、苇子坪洞沟-剪子沟地区等为近期的找矿重点地区,并对长沟-洞沟地区、梯子崖—三角崖地区指出了具体的找矿方向,认为长沟-洞沟地区的已知铅锌矿带与八卦庙金矿床处于同一次级热水沉积盆地中,其范围大致与河-2异常吻合,成矿条件良好,长沟背斜南翼(倒转翼)、倾伏端和洞沟背斜长沟—八卦庙段是下一步铅锌金的重要找矿地段。这些对该区的找矿工作具有重要的指导意义。
    Abstract: On the base of comprehensively researching regional geological background, geochemical and geophysical characteristics in Feng-Tai multi-metal ore cluster region and combined with systematicly analyzing discovered mineral deposits here, there could be divided into three metallogenic series, including Devonian carbonate rock-hosted lead and zinc deposit metallogenic series, Devonian sedimentary reformation typed copper deposit metallogenic series, and Mesozoic orogenesis-related gold deposit metallogenic seried. It is concluded that Changgou-Donggou,Qiliping in Fengzhou and Weiziping-Donggou-Jianzigou region are very important for exploration in the nearfuture,and point clear prospecting direction for Changgou-Donggou,Tiziya-Sanjiaoya region. It is considered that discovered lead and zinc zone in Changgou-Donggou located in the same secondary hydrothermal sedimentary ba sin with Baguamiaogold deposit,which range coincide with that of He-2 anomaly,where hase good metallogen ic condition. South limb(overturned limb)and plunging end of Changgou anticline and Changgou-Baguamiao segment of Donggou anticline are animportan texploration target for lead,zinc and gold. These have important significance to guide exploration work in Feng-Tairegion.
  • 方维萱,刘方杰,胡瑞忠,等.凤太泥盆纪拉分盆地中硅质铁白云岩-硅质岩特征及成岩成矿方式[J].岩石学报,2000,16(4):700-710.

    李发林,王瑞廷,陈二虎.凤-太矿田大型铅锌矿床勘查靶区及其找矿思路[J].西北地质,2004,37(3):56-60.

    李文渊,董福辰,姜寒冰,等.西北地区重要金属矿产成矿特征及其找矿潜力[J].西北地质,2006,39(2):1-16.

    刘方杰,裴先治,孙勇.陕西凤县八卦庙金矿床脆-韧性剪切构造及其控矿特征[J].西北大学学报(自然科学版),1999,29(6):569-574.

    毛景文,李晓峰,张荣华,等.深部流体成矿系统.北京:中国大地出版社[M],2005,269-320.

    王瑞廷.秦岭造山带泥盆系陕西段主要金矿床地球物理地球化学异常特征及找矿标志[J].物探与化探,1999,23(1):14-20.

    王瑞廷.秦岭造山带陕西段主要矿集区典型金属矿床成矿模式和找矿预测研究[R].北京:中国地质大学,2005,1-173.

    王集磊,何伯墀,李建中,等.中国秦岭型铅锌矿床[M].北京:地质出版社,1996,1-108.

    王相,唐荣扬,李实,等.秦岭造山与金属成矿[M].北京:冶金工业出版社,1996,1-326.

    薛春纪.秦岭泥盆纪热水沉积[M].西安:西安地图出版社,1997,1-134.

    钟建华.陕西秦岭泥盆系区域成矿大地构造演化背景与八卦庙金矿的成因及控矿构造的研究[R].西安:西北大学,1995,1-99.

    钟建华.陕西秦岭泥盆系区域成矿大地构造演化[J].大地构造与成矿学,1997,21(3):242-250.

    FANG Weixuan,LIU Fangjie,HU Ruizhong,et al.Silicic ankerite and silicalite feature,rock-forming and ore-forming ways in Devonian pulled-separated basin,Feng-Tai region[J].Acta Petrologica Sinica,2000,16(4):700-710 (in Chinese with English abstract).

    LI Falin,WNG Ruiting,CHEN Erhu,et al.Exploration target area for large-scale Lead and zinc deposit and its prospecting thoughts in Fengxian-Taibai Ore Field,Shaanxi Province[J].Northwest Geology,2006,39(2):56-60 (in Chinese with English abstract).

    LI Wenyuan,DONG Fuchen,JIANG Hanbing,et al.Metallogenetic characteristics and prospecting potential of major metallic minerals in Northwest China[J].Northwest Geology,2006,39(2):1-16 (in Chinese with English abstract).

    LIU Fangjie,PEI Xianzhi,SONG Yong.Brittle-ductile shear structure and its ore-controlled characteristics of Baguamiao gold deposit,Feng county,Shannxi Province[J].Journal of Northwest University (natural science edition) 1999,29(6):569-574 (in Chinese with English abstract).

    MAO Jingwen,LI Xiaofeng,ZHANG Ronghua,et al.Deep fluid metallogenic system[M].Land Publishing House,Beijing,2005,269-320 (in Chinese with English abstract).

    WANG Ruiting.Geophysical and geochemical anomaly characteristics and exploration indicator of main gold ore deposits in Devonian system of Qinling orogenic belt in Shannxi Province,China[J].Geophysical and Geochemical Exploration,1999,23(1):14-20 (in Chinese with English abstract).

    WANG Ruiting.Study on metallogenic model for typic metal ore deposits and exploration predicting of Qinling orogenic belt in Shannxi Province,China[R].China University of Geosciences,Beijing,2005,1-173(in Chinese with English abstract).

    WANG Jilei,HE Bochi,LI Jianzhong,et al.Qinling type lead and zinc mineral deposits in China[M].Geological Publishing House,Beijing,1996,1-108 (in Chinese with English abstract).

    WANG Xiang,TANG Rongyang,LI Shi,et al.Qinling orogeny and metallogenesis[M].Metallurgical Industry Press,Beijing,1996,12-326 (in Chinese with English abstract).

    XUE Chunji.Devonian hydrothermal sedimentation in Qinling area,China[M].Xi'an Cartographic Pblishing House,Xi'an,1997,1-134 (in Chinese with English abstract).

    ZHONG Jianhua.Study on regional metallogenesis geotectonic evolution setting of Devonian system in Qinling area and genesis and ore-controlled structure of Baguamiao gold deposit,Shannxi Province[R].Northwest University,Xi'an,1995,1-99 (in Chinese with English abstract).

    ZHONG Jianhua.Regional metallogenesis geotectonic evolution of Devonian system in Qinling area,Shannxi Province[J].Geotectonica et Metallogenia,1997,21(3):242-250 (in Chinese with English abstract).

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出版历程
  • 收稿日期:  2007-05-17
  • 修回日期:  2007-06-07
  • 发布日期:  2007-06-04

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