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滇东南都龙锡锌铟多金属矿床构造控矿模式及找矿方向

薛伟 张达 李成远 方烨 陈子丹

薛伟, 张达, 李成远, 等, 2019. 滇东南都龙锡锌铟多金属矿床构造控矿模式及找矿方向. 地质力学学报, 25 (1): 77-89. DOI: 10.12090/j.issn.1006-6616.2019.25.01.008
引用本文: 薛伟, 张达, 李成远, 等, 2019. 滇东南都龙锡锌铟多金属矿床构造控矿模式及找矿方向. 地质力学学报, 25 (1): 77-89. DOI: 10.12090/j.issn.1006-6616.2019.25.01.008
XUE Wei, ZHANG Da, LI Chengyuan, et al., 2019. STRUCTURAL ORE-CONTROLLING MODEL AND PROSPECTING RESEARCH FOR THE DULONG SN-ZN-IN POLYMETALLIC DEPOSIT, SOUTHEASTERN YUNNAN. Journal of Geomechanics, 25 (1): 77-89. DOI: 10.12090/j.issn.1006-6616.2019.25.01.008
Citation: XUE Wei, ZHANG Da, LI Chengyuan, et al., 2019. STRUCTURAL ORE-CONTROLLING MODEL AND PROSPECTING RESEARCH FOR THE DULONG SN-ZN-IN POLYMETALLIC DEPOSIT, SOUTHEASTERN YUNNAN. Journal of Geomechanics, 25 (1): 77-89. DOI: 10.12090/j.issn.1006-6616.2019.25.01.008

滇东南都龙锡锌铟多金属矿床构造控矿模式及找矿方向

doi: 10.12090/j.issn.1006-6616.2019.25.01.008
基金项目: 

国家重点研发计划 2016YFC0600509

中央高校基本科研业务费专项资金资助 2652017259

详细信息
    作者简介:

    薛伟(1990-), 男, 在读博士, 构造地质学专业。E-mail:xueweiwd@163.com

    通讯作者:

    张达(1967-), 男, 教授, 主要从事构造地质学与区域成矿规律研究。E-mail:zhangda@cugb.edu.cn

  • 中图分类号: P618.2

STRUCTURAL ORE-CONTROLLING MODEL AND PROSPECTING RESEARCH FOR THE DULONG SN-ZN-IN POLYMETALLIC DEPOSIT, SOUTHEASTERN YUNNAN

  • 摘要: 都龙锡锌铟多金属矿床位于华南板块西南缘之滇东南老君山矿集区南部,是中国重要的锡锌铟多金属资源产地,构造控矿特征明显。对铜街、曼家寨两个典型矿段及外围构造变形分析及控矿构造解析表明:区内各地质体之间均为构造接触,构造变形主要存在伸展滑脱及左行走滑等构造样式;F0、F1、F2三条南北向断裂组成的早白垩世伸展滑脱构造控制了矿区的矿化蚀变及矿体空间产出形态,是矿区最主要的控矿构造;成矿后北西向马关—都龙左行走滑断裂为破矿构造,但其正断的性质使矿区受剥蚀程度相对较低,对矿床保存有利。根据控矿构造组合特征及区域构造背景建立了构造控矿模式,认为矿区南部深部、西部寒武系地层与新寨岩组深部为进一步寻找锡锌铟矿的有利区域,矿区深部找矿潜力较大。

     

  • 图  1  都龙矿区区域地质图及其大地构造位置图[2, 14, 20]

    a—研究区大地构造位置;b—Songchay变质穹窿区域构造格架;c—都龙矿区及外围区域地质图

    Figure  1.  Geological map and geotectonic location of the Dulong Sn-Zn-In deposit[2, 14, 20]

    图  2  都龙矿区南部五口硐一带AB剖面图(位置见图 1)

    1—燕山晚期花岗斑岩脉;2—南温河片麻状花岗岩;3—寒武系中统龙哈组白云质灰岩、千枚岩;4—寒武系中统田蓬组大理岩、千枚岩;5—新元古界新寨岩组石英片岩夹碳酸盐岩透镜体;6—古元古界南秧田岩组片岩

    Figure  2.  The Wukoudong section AB in the south of the Dulong district (location in figure 1)

    图  3  都龙矿区曼家寨矿段15号勘探剖面线

    1—Sn-Zn-In矿体;2—断层;3—新寨岩组;4—钻孔位置及深度;5—南温河片麻状花岗岩;6—地质界限;7—老君山岩体;8—大理岩;9—石英片岩;10—夕卡岩

    Figure  3.  Geological sections along exploration line 15 of the Dulong deposit

    图  4  都龙矿区典型矿石照片

    Fl—萤石;Act—阳起石;Grt—石榴子石;Sp—闪锌矿;Py—黄铁矿;Ccp—黄铜矿;Qtz—石英a—萤石阳起石夕卡岩矿石;b—石榴子石夕卡岩;c—黄铁矿闪锌矿阳起石夕卡岩;d—石英脉型矿石

    Figure  4.  Photographs of typical ores in the Dulong deposit

    图  5  矿区东部F0断裂变形特征(红色箭头指示断层上盘运动方向,灰色箭头指示断层下盘运动方向)

    a—F0断面展布特征(平行断面);b—F0断面变形特征(垂直断面);c—F0断面波状起伏;d—断面发育阶步及擦痕

    Figure  5.  Deformation characteristics of the F0 fault

    图  6  曼家寨矿段1180平台F1断裂变形特征

    a—F1断裂展布及其它照片位置;b—滑脱褶皱构造;c—大理岩夹石发生褶皱变形;d—夕卡岩发生褶皱变形;e—断裂带内次级断裂面擦痕

    Figure  6.  Deformation characteristics of the F1 fault

    图  7  F2断裂构造变形特征

    a—F2断裂野外照片;b—F2断裂野外素描图;c—F2断裂局部放大图;d—断层上盘寒武系地层发生褶皱变形

    Figure  7.  Deformation characteristics of the F2 fault

    图  8  马关—都龙断裂构造变形特征

    a—铜街北部马关—都龙断裂野外照片;b—阶步、擦痕及垂直断面发育的张性方解石脉;c—书斜构造

    Figure  8.  Deformation characteristics of the Maguan-Dulong fault

    图  9  都龙矿区不同类型控矿构造特征及矿体形态

    a—背斜鞍部产出矿体;b—张性空间内矿体;c—“Y”字形次级断裂控制矿体;d—复合断裂控制矿体产出;e—褶皱控制矿体产出;f—断裂带下盘产出矿体;g—似层状矿体;h—次级断裂控制矿体;i—断裂带内产出矿体

    Figure  9.  Different types of ore-controlling structure features and the ore body morphology

    图  10  都龙锡锌铟矿构造控矿模式图

    Figure  10.  Structural ore-controlling model of the Dulong Sn-Zn-In deposit

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  • 收稿日期:  2018-06-14
  • 修回日期:  2018-10-19
  • 刊出日期:  2019-02-01

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