贵州深部四级断裂构造特征及与重要矿产的关系

王亮; 胡从亮; 张嘉玮; 陈国勇

doi:10.12090/j.issn.1006-6616.2019.25.01.005

贵州深部四级断裂构造特征及与重要矿产的关系

doi: 10.12090/j.issn.1006-6616.2019.25.01.005

王亮^{1, 2,},
胡从亮¹,
张嘉玮^{1, 2, ,},
陈国勇³

1.
贵州省地质调查院, 贵州贵阳 550081
2.
贵州省地质物探开发应用工程技术研究中心, 贵州贵阳 550081
3.
贵州省地质矿产勘查开发局, 贵州贵阳 550004

基金项目: 贵州省地质矿产勘查开发局重大科研专项(黔地矿纪要(2015)14号); 黔科合平台人才[2018]5626;黔科合J字[2015]2081;黔科合平台人才[2017]5739;黔科合[2016]平台人才5401

详细信息

作者简介:
王亮(1962-), 男, 研究员, 主要从事地球物理勘查和重磁方面研究工作。E-mail:wangliang62@163.com

通讯作者:
张嘉玮(1986-), 男, 高级工程师, 博士后, 主要从事固体矿产勘查和研究工作。E-mail:jiaweizhang@live.cn

中图分类号: P542;P618
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- 被引次数: 0
出版历程
- 收稿日期: 2018-07-26
- 修回日期: 2018-12-25
- 刊出日期: 2019-02-01

CORRELATION BETWEEN THE STRUCTURAL CHARACTERISTICS OF THE DEEP FOUR-LEVEL FAULT AND THE IMPORTANT MINERAL DEPOSITS IN GUIZHOU PROVINCE

WANG Liang^{1, 2
,},
HU Congliang¹,
ZHANG Jiawei^{1, 2
, ,},
CHEN Guoyong³

1.
Guizhou Institute of Geological Survey, Guiyang 550081, Guizhou, China
2.
Guizhou Engineering Research Center for Geologic-Geophysical Exploration Development and Application, Guiyang 550081, Guizhou, China
3.
Bureau of Geology and Mineral Exploration and Deuelopment of Guizhou Province, Guiyang 550004, Guizhou, China

摘要

摘要: 贵州位于扬子陆块、江南造山带、右江造山带的复合部位，自新元古代以来，发生了多次重要的构造伸展运动和构造挤压变形。晚古生代之后的沉积活动，掩盖了早期地质构造形迹。多位学者曾对贵州的深部断裂进行过推断，但由于资料不足、认识差异等原因，研究存在局限和争议。在充分借鉴已有研究成果的基础上，通过综合应用重力、航磁、地质等资料，提取了贵州深部四级断裂构造体系。所推测的贵州深部Ⅰ级断裂3条，呈"H型"结构；Ⅱ级断裂15条、Ⅲ级断裂12条，基底断裂若干条，这些断裂均在上一级断裂的基础上发展演化。根据人工地震剖面资料，进一步验证了5条深部Ⅰ至Ⅲ级断裂的展布特征，发现这些断裂沿不同倾向延伸、切割深度达6~12km，为切穿沉积盖层和基底的深大断裂。结合四级断裂构造体系及贵州省内重要矿产的分布，提出贵州金、铅锌、锑、锰、磷、铝土矿分布与Ⅰ、Ⅱ、Ⅲ级深部断裂构造具有空间联系。
- 梯度带 /
- 深大断裂 /
- 基底断裂 /
- 重要矿产 /
- 贵州
Abstract: Guizhou Province is located at the convergent parts of the Yangtze Plate, Jiangnan Orogen and Youjiang Orogen. Several major tectonic extensions and structural deformation due to tectonic compressions have taken place since the Neoproterozoic Era. However, the sedimentation that occurred after the late Paleozoic Era had covered those early geological structures. Studies on the deduction of the deep fractures in Guizhou Province by several authors are still limited in scope and controversial due to the insufficient data and differences in perception. In this paper, the deep four-level fault in Guizhou Province was classified with a combined application of gravity, aeromagnetic survey technologies, and geological data, which is supported strongly by the existing studies. According to the deduced results, other than the three pieces of deep Level Ⅰ fractures, which had "H-shaped" structures, 15 pieces of Level Ⅱ fractures, 12 pieces of Level Ⅲ fractures, and several pieces of basement fractures were also found. It was also deduced that each of the said fractures was resulted by the development of the fracture-level right above it. According to the artificial seismic profile, the distribution characteristics of five of the fault pieces from Level Ⅰ to Ⅲ have been tested further. The results showed that those fractures were extended to different directions and the cutting depth had reached 6~12 km. To conclude, the fractures' profile as deep fractures, which cut through the sedimentary mantle and basement, had been confirmed. Furthermore, combining the knowledge of the four-level fault and the distribution of important mineral deposits in Guizhou Province, a deduction was put forward, wherein a spatial correlation that linked the distribution of the gold, lead and zinc, antimony, manganese, phosphorus, and bauxite ores in Guizhou Province with the Level Ⅰ, Ⅱ, and Ⅲ deep fractures might have existed.
- gradient zone /
- deep fault /
- basement fault /
- important mineral /
- Guizhou
注释:

责任编辑：吴芳

HTML全文

图 1 贵州省地质构造略图^[7]

I—贵州侏罗山式褶皱带：(I1—武陵山NNE向褶皱冲断带；I2—毕节及安顺NE向变形带；I3—乌蒙山NW向走滑变形带)；Ⅱ—江南造山型褶皱带；Ⅲ—右江造山型褶皱带；Ⅳ—四川盆地边缘平缓开阔褶皱区；Fa—施洞口断裂; Fb—南盘江断裂; Fc—习水断裂; F0—望谟—贵阳—遵义断裂; F1—安顺—贵阳—镇远断裂; F2—普安—安顺断裂; F3—水城—紫云—罗甸断裂

Figure 1. The geological structure map of Guizhou province^[7]

下载: 全尺寸图片幻灯片

图 2 不同时期划分的贵州深部地质构造^[8~12]

Figure 2. Different demarcations on the deep faults of Guizhou province^[8~12]

下载: 全尺寸图片幻灯片

图 3 QZ04-80线地震剖面A-A′垭都—紫云断裂带(据文献[12]修编)

a—断裂显示图；b—地质解释剖面图

Figure 3. Display map of Yadu-Ziyun fault zone in QZ04-80 linar seismic profile(A-A′) (modified from reference [12])

下载: 全尺寸图片幻灯片

图 4 贵州莫霍面等深线与重力、航磁异常推测深部(Ⅰ级—Ⅲ级)断裂及对应关系

Figure 4. Correlation between Moho isobaths and deep fault (Level Ⅰ to Ⅲ) speculated by gravity anomaly and aeromagnetic anomaly in Guizhou province

下载: 全尺寸图片幻灯片

图 5 贵州重力、航磁异常推测深部(Ⅰ级—Ⅳ级)断裂及与重要矿产分布关系

1—推测Ⅰ级深部断裂；2—推测Ⅱ级深部断裂；3—推测Ⅲ级深部断裂；4—推测基底断裂；5—金矿；6—铝土矿；7—锰矿；8—锑矿；9—铅锌矿；10—磷矿

Figure 5. Correlation between deep faults (Level Ⅰ to Ⅳ) speculated by gravity anomaly and aeromagnetic anomaly and the important mineral deposits in Guizhou province

下载: 全尺寸图片幻灯片

参考文献(37)

[1]	曾帅. "在贵州做科研, 大有作为!"——贵州省科学技术奖励大会侧记[N].贵州日报, 2018~07~13(01). ZENG Shuai. "Doing scientific research Guizhou Province is fulfilled" A brief of the Science and Technology Award Conference of Guizhou Province[N] Guizhou Daily, 2018~07~13(01). (in Chinese)
[2]	林小会, 何良伦, 秦文博.赫章发现我省首个超大型铅锌矿床[N].贵州地矿报, 2018~08~01. LIN Xiaohui, HE Lianglun, QIN Wenbo. Hezhang County discovered the first super large Pb-Zn deposit in Guizhou Province[N]. Newspaper of Bureau of Geology and Mineral Resources, 2018~08~01. (in Chinese)
[3]	周丽娜, 张兵强.贵州地矿105队发现贵州玄武岩地区最大原生金矿[N].贵州地矿报, 2018~07~05. ZHOU Li'na, ZHANG Bingqiang. Discovery of the largest primary gold deposit in basalt area of Guizhou Province by No. 105 Geological team of Bureau of Geology and Mineral Resources[N]. Newspaper of Bureau of Geology and Mineral Resources, 2018~07~05. (in Chinese)
[4]	余杰, 徐阳东, 田亚江, 等.贵州省丹寨老东寨铅锌矿床地质特征及控矿条件分析[J].贵州地质, 2018, 35(1):14~19. doi: 10.3969/j.issn.1000-5943.2018.01.003 YU Jie, XU Yangdong, TIAN Yajiang, et al. Geologic characteristic and analysis on ore-controlling factors of Laodongzhai lead-zinc deposit in Danzhai, Guizhou Province[J]. Guizhou Geology, 2018, 35(1):14~19. (in Chinese with English abstract) doi: 10.3969/j.issn.1000-5943.2018.01.003
[5]	贵州省地质局.贵州省区域地质志[M].北京:地质出版社, 1987. Guizhou Bureau of Geology and Mineral Resources. Regional geology of Guizhou province[M]. Beijing:Geological Publishing House, 1987. (in Chinese)
[6]	程裕淇.中国区域地质概论[M].北京:地质出版社, 1994. CHENG Yuqi. An introduction to the regional geology of China[M]. Beijing:Geological Publishing House, 1994. (in Chinese)
[7]	王砚耕.贵州区域构造矿田构造学术讨论会论文集——贵州构造基本格架及其特征[M].贵阳:贵州科技出版社, 1992, 1~11. WANG Yangeng. Guizhou regional tectonic structure of academic discussion of the causes of proceedings-The tectonics framework in Guizhou Province and its characteristics[M]. Guiyang:Guizhou Science and Technology Press, 1992, 1~11. (in Chinese)
[8]	齐涿.贵州区域重力场基本特征和初步分析[J].贵州地质科技情报, 1981, 1(1):32~36. QI Zhuo. Basic characteristics and preliminary analysis of regional gravity field in Guizhou Province[J]. Guizhou Geological Science and Technology Information, 1981, 1(1):32~36. (in Chinese)
[9]	范祥发.从1:50万重力异常探讨贵州省区域地质构造格架[J].贵州地质, 1999, 16(3):195~198. http://d.old.wanfangdata.com.cn/Periodical/wts201506008 FAN Xiangfa. Discussion on the regional geological tectonic framework of Guizhou based on 1:500000 gravity anomaly[J]. Guizhou Geology, 1999, 16(3):195~198. (in Chinese with English abstract) http://d.old.wanfangdata.com.cn/Periodical/wts201506008
[10]	王亮, 龙秀洪, 张应文, 等.贵州1:20万重力异常分布特征与透露的区域地质构造新信息[J].贵州地质, 2007, 24(1):64~69. doi: 10.3969/j.issn.1000-5943.2007.01.013 WANG Liang, LONG Xiuhong, ZHANG Yingwen, et al. Distribution characteristics of gravity anomaly with a scale of 1 to 200, 000 and new information exposed on regional geologic structure in Guizhou[J]. Guizhou Geology, 2007, 24(1):64~69. (in Chinese with English abstract) doi: 10.3969/j.issn.1000-5943.2007.01.013
[11]	戴传固, 秦守荣, 陈建书, 等.试论贵州深部隐伏断裂特征[J].地质科技情报, 2013, 32(6):1~6. http://www.cqvip.com/QK/93477A/201306/47781818.html DAI Chuangu, QIN Shourong, CHEN Jianshu, et al. Characteristics of deep concealed faults in Guizhou[J]. Geological Science and Technology Information, 2013, 32(6):1~6. (in Chinese with English abstract) http://www.cqvip.com/QK/93477A/201306/47781818.html
[12]	吴开彬, 曾广乾, 陈国雄, 等.布格重力异常揭示的贵州深部构造特征[J].地质科技情报, 2016, 35(1):190~199. http://d.old.wanfangdata.com.cn/Conference/8159390 WU Kaibin, ZENG Guangqian, CHEN Guoxiong, et al. Deep structural features of Guizhou revealed by Bouguer gravity anomaly[J]. Geological Science and Technology Information, 2016, 35(1):190~199. (in Chinese with English abstract) http://d.old.wanfangdata.com.cn/Conference/8159390
[13]	周雁.垭都-紫云-罗甸断裂带及其对两侧盆地成藏条件影响研究[R].成都: 中国石油化工股份有限公司石油勘探开发研究院, 2008. ZHOU Yan. Study on the Yadu-Ziyun-Luodian fault zone and its influence on the reservoir forming conditions of the basins on both sides[R]. Chengdu: Petroleum Exploration and Development Research Institute of China Petrochemical Co., Ltd., 2008. (in Chinese)
[14]	汪新伟, 郭彤楼, 沃玉进, 等.垭紫罗断裂带深部构造分段特征及构造变换作用[J].石油与天然气地质, 2013, 34(2):220~228. http://d.old.wanfangdata.com.cn/Periodical/syytrqdz201302013 WANG Xinwei, GUO Tonglou, WO Yujin, et al. Characteristics of deep structural segmentation and transformation of the Yaziluo fault zone[J]. Oil and Gas Geology, 2013, 34(2):220~228. (in Chinese with English abstract) http://d.old.wanfangdata.com.cn/Periodical/syytrqdz201302013
[15]	毛健全, 张启厚, 顾尚义.水城断陷的地质特征及构造演化[J].贵州工业大学学报, 1997, 26(2):1~6. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199700163238 MAO Jianquan, ZHANG Qihou, GU Shangyi. The geological characteristics and tectonic evolution of Shuicheng fault subsidence[J]. Journal of Guizhou University of Technology, 1997, 26(2):1~6. (in Chinese with English abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199700163238
[16]	孙文珂, 黄崇轲, 丁鹏飞.应用物探资料研究:重点成矿区带的区域构造和成矿构造文集-中国东南大陆深部地质构造与区内若干重要矿田的关联[M].北京:地质出版社, 2001. SUN Wenke, HUANG Chongke, DING Pengfei. Application of Geophysical data to the study of regional structures and metallogenic structures in key metallogenic zones-Relationship between deep geological structure and some important ore fields in southeastern China[M]. Beijing:Geological Publishing House, 2001. (in Chinese)
[17]	黔桂滇重点片综合解释组.黔桂滇重点片综合解释成果报告[R].地矿部华南地区物探化探遥感成果编图委员会, 1995. Integrated Interpretation Team of Guizhou, Guangxi and Yunnan Key Area. A report on the comprehensive interpretation of Guizhou, Guangxi and Yunnan key area[R]. Mapping Committee of Geophysical and Geochemical and Remote Sensing of South China, Ministry of Geology and Mineral Resources, 1995. (in Chinese)
[18]	孙文珂, 金宜声, 涂承林, 等.应用物探资料研究:重点成矿区带的区域构造和成矿构造文集-中国及其毗邻海区重力系列图读图说明[M].北京:地质出版社, 2001. SUN Wenke, JIN Yisheng, TU Chenglin, et al. Application of Geophysical data to the study of regional structures and metallogenic structures in key metallogenic zones-Directions for a series of gravity anomaly maps of land and seas of China[M]. Beijing:Geological Publishing House, 2001. (in Chinese)
[19]	张明华, 乔计花, 刘宽厚, 等.重力资料解释应用技术要求[M].北京:地质出版社, 2010. ZHANG Minghua, QIAO Jihua, LIU Kuanhou, et al. Gravity data interpretation technology application requirements[M]. Beijing:Geological Publishing House, 2010. (in Chinese)
[20]	范正国, 黄旭钊, 熊盛青, 等.磁测资料应用技术要求[M].北京:地质出版社, 2010. FAN Zhengguo, HUANG Xuzhao, XIONG Shengqing, et al. Technical requirements for magnetic data application[M]. Beijing:Geological Publishing House, 2010. (in Chinese)
[21]	湖南省地质调查院.湖南省区域地质志[R].长沙: 湖南省地质调查院, 2012. Hunan Institute of Geological Survey. Regional geology of Hunan province[M]. Changsha: Hunan Institute of Geological Survey, 2012. (in Chinese)
[22]	广西地质调查院.广西区域地质志[R].南宁: 广西地质调查院, 2012. Guangxi Institute of Geological Survey. Regional geology of Guangxi province[R]. Nanning: Guangxi Institute of Geological Survey, 2012. (in Chinese)
[23]	朱介寿, 蔡学林, 曹家敏, 等.中国华南及东海地区岩石圈三维结构及演化[M].北京:地质出版社, 2005. ZHU Jieshou, CAI Xuelin, CAO Jiamin, et al. The three dimension structure of lithosphere and its evolution in South China and East China Sea[M]. Beijing:Geological Publishing House, 2005. (in Chinese)
[24]	周振昊, 杜远生.贵州铜仁枫木寨隐爆角砾岩筒的发现及地质意义[J].地质科技情报, 2013, 32(1):94~98. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK201300121378 ZHOU Zhenhao, DU Yuansheng. Discovery and geological significance of the Cryptoexplosive breccia rock pipe in Fengmuzhai, Tongren, Guizhou Province[J]. Geological Science and Technology Information, 2013, 32(1):94~98. (in Chinese with English abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK201300121378
[25]	曾华霖.重力场与重力勘探[M].北京:地质出版社, 2005. ZENG Hhalin. Gravity field and gravity exploration[M]. Beijing:Geological Publishing House, 2005. (in Chinese)
[26]	金文山, 赵凤清, 张慧民, 等.华南大陆深部地壳结构及其演化[M].北京:地质出版社, 1997. JIN Wenshan, ZHAO Fengqing, ZHANG Huimin, et al. Deep crustal structure and evolution of South China continent[M]. Beijing:Geological Publishing House, 1997. (in Chinese)
[27]	王尚彦.贵州的断裂与地震[J].地质力学学报, 2016, 22(3):430~438. doi: 10.3969/j.issn.1006-6616.2016.03.004 WANG Shangyan. Faults and earthquakes in Guizhou[J]. Journal of Geomechanics, 2016, 22(3):430~438. (in Chinese with English abstract) doi: 10.3969/j.issn.1006-6616.2016.03.004
[28]	云南省地质矿产局.云南省区域地质志[M].北京:地质出版社, 1987. Yunnan Bureau of Geology and Mineral Resources. Regional geology of Guizhou province[M]. Beijing:Geological Publishing House, 1987. (in Chinese)
[29]	贵州省地质调查院.中国区域地质志·贵州志[M].北京:地质出版社, 2017. Guizhou Institute of Geological Survey. The first advisory committee of the Regional Geology of China·Guizhou province[M]. Beijing:Geological Publishing House, 2017. (in Chinese)
[30]	郭卫星, 熊亮, 魏力民.川东南构造变形特征及其对页岩气保存的影响[J].煤田地质与勘探, 2016, 44(6):21~26. doi: 10.3969/j.issn.1001-1986.2016.06.004 GUO Weixing, XIONG Liang, WEI Limin. Structure deformation of southeast Sichuan and its influences on preservation of shale gas[J]. Coal Geology and Exploration, 2016, 44(6):21~26. (in Chinese with English abstract) doi: 10.3969/j.issn.1001-1986.2016.06.004
[31]	张岳桥, 董树文, 李建华, 等.中生代多向挤压构造作用与四川盆地的形成和改造[J].中国地质, 2011, 38(2):233~250. doi: 10.3969/j.issn.1000-3657.2011.02.001 ZHANG Yueqiao, DONG Shuwen, LI Jianhua, et al. Mesozoic multi-directional compressional tectonics and formation-reformation of Sichuan basin[J]. Geology in China, 2011, 38(2):233~250. (in Chinese with English abstract) doi: 10.3969/j.issn.1000-3657.2011.02.001
[32]	高军波, 杨瑞东.水城-紫云-南丹深大断裂构造演化与泥盆纪热水(液)成岩、成矿效应[M].贵阳:贵州科技出版社, 2015. GAO Junbo, YANG Ruidong. Tectonic evolution of Shuicheng-Ziyun-Nandan deep fault and diagenesis and mineralization of Devonian hot water (liquid)[M]. Guiyang:Guizhou Science and Technology Press, 2015. (in Chinese)
[33]	刘家铎, 张成江, 李佑国, 等.扬子地台西南缘成矿规律及找矿方向综合研究报告[R].成都: 成都理工大学, 2003. LIU Jiaduo, ZHANG Chengjiang, LI Youguo, et al. A comprehensive research report on metallogeny and prospecting direction of the southwest margin of the Yangtze platform[R]. Chengdu: Chengdu University of Technology, 2003. (in Chinese)
[34]	张荣强, 周雁, 汪新伟, 等.贵州西南部威-紫-罗断裂带构造特征及演化[J].地质力学学报, 2009, 15(2):178~189. doi: 10.3969/j.issn.1006-6616.2009.02.007 ZHANG Rongqiang, ZHOU Yan, WANG Xinwei, et al. Structural features and tectonic evolution of the Wei-Zi-Luo fault zone in Southwestern Guizhou Province[J]. Journal of Geomechanics, 2009, 15(2):178~189. (in Chinese with English abstract) doi: 10.3969/j.issn.1006-6616.2009.02.007
[35]	王尚彦, 张慧, 彭成龙, 等.贵州西部古-中生代地层及裂陷槽盆的演化[M].北京:地质出版社, 2005. WANG Shangyan, ZHANG Hui, PENG Chenglong, et al. Strata of Palaeozoic-Mesozoic and evolution of the Chasmic furrow in Western Guizhou Province[M]. Beijing:Geological Publishing House, 2005. (in Chinese)
[36]	郭良辉, 高锐, 张季生, 等.新元古代扬子-华夏陆块拼合带:来自华南重磁异常的启示[J].地质科学, 2016, 51(3):682~693. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzkx201603002 GUO Lianghui, GAO Rui, ZHANG Jisheng, et al. The geosuture between the Yangtze and Cathaysia blocks, South China, during Neoproterozoic era revealed from gravity and magnetic data[J]. Chinese Journal of Geology, 2016, 51(3):682~693. (in Chinese with English abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzkx201603002
[37]	孙文珂, 黄崇柯, 丁鹏飞, 等.应用物探资料研究:重点成矿区带的区域构造和成矿构造文集-钦州-钱塘结合带及其控矿作用[M].北京:地质出版社, 2001, 75~102. SUN Wenke, HUANG Chongke, DING Pengfei, et al. Application of Geophysical data to the study of Regional structures and metallogenic structures in key metallogenic zones-Qinzhou-Qiantang belt and its ore-controlling process[M]. Beijing:Geological Publishing House, 2001, 75~102. (in Chinese)