东川运动及其对东川矿区褶皱构造的影响

刘卫明; 刘继顺; 尹利君; 杨立功; 刘文恒; 豆松

东川运动及其对东川矿区褶皱构造的影响

刘卫明^{1, 2,},
刘继顺¹,
尹利君¹,
杨立功¹,
刘文恒¹,
豆松^{1, 3}

1.
中南大学地球科学与信息物理学院, 长沙 410083
2.
江西理工大学资源与环境工程学院, 江西赣州 341000
3.
云南省有色地质勘查局, 昆明 650051

基金项目:

云南省省院省校合作项目 2003UDBEA00A026

详细信息

作者简介:
刘卫明(1964-), 男, 博士研究生, 教授, 主要从事矿业信息化和矿山地质教学研究工作。E-mail:wm_liu@sina.com

中图分类号: P542
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- 被引次数: 0
出版历程
- 收稿日期: 2011-10-24
- 刊出日期: 2012-03-01

DONGCHUAN MOVEMENT AND ITS INFLUENCE ON FOLDING STRUCTURES IN DONGCHUAN MINING DISTRICT

1.
School of Geosciences and Info-Physics, Central South University, Changsha 410083, China
2.
Faculty of Resources and Environmental Engineering, Jiangxi University of Science and Technology, Ganzhou 341000, China
3.
Yunnan Non-ferrous Metal Geological Exploration Bureau, Kunming 650051, China

摘要

摘要: 分析了当前东川运动的各种认识，通过上下地层的特征、构造、变质作用、火山-岩浆活动、形成背景以及汤丹、落雪和拖布卡3个典型剖面的研究，确定该运动是一次大规模的构造运动。东川运动是南北向挤压运动，在东川矿区下（昆阳）亚群形成东西向褶皱构造，被后期小黑箐和晋宁运动叠加改造后，其构造形迹变得模糊和复杂，但经仔细研究分辨出了10个较大的褶皱构造。
- 东川运动 /
- 褶皱构造 /
- 昆阳群 /
- 东川矿区
Abstract: The various understandings about Dongchuan Movement were analyzed. Researches on characteristics of the strata in Kunyang Group, metamorphism, volcano-magma activities, and typical profiles as Tangdan, Luoxue and Tuobuka show that Dongchuan Movement is a large-scale tectonic movement. Dongchuan Movement is SN-trend compressional movement. In Dongchuan mining district, EW-trend fold structures formed in the lower Kunyang subgroup. These EW-trend fold structures were reformed and transformed by later Xiaoheijing Movement and Jinning Movement. The structural features became indistinct and complex. But after a careful study, the 10 larger fold structures were distinguished in Dongchuan mining district.
- Dongchuan Movement /
- folding structure /
- Kunyang Group /
- Dongchuan mining district

HTML全文

图 1 东川矿区地质构造纲要图

1—古元古界（Pt₁）；2—中元古界（Pt₂）；3—新元古界澄江组（Pt₃c）；4—新元古界灯影组（Pt₃dn）；5—边界断层；6—同生断层；7—向斜轴、倾没端；8—背斜轴、倾没端；9—河流；10—古火山口；11—火山角砾岩；a—小江断层；b—普渡河断层；c—麻塘断层；d—宝九断层

Figure 1. Geological structure outline map of Dongchuan deposit

下载: 全尺寸图片幻灯片

图 2 因民组（Pt₂ky）与平顶山组（Pt₁kp）不整合接触（据文献[11]修改）

Figure 2. Unconformable contact of Yinmin Formation and Pingdingshan Formation

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图 3 宝台厂—马柱硐构造剖面略图

Figure 3. The outline map of Baotaichang-Mazhudong tectonic profile

下载: 全尺寸图片幻灯片

参考文献(20)

[1]	段嘉瑞, 刘继顺, 胡祥昭. 云南东川铜矿区1: 5万地质图修编及成矿预测研究[R]. 长沙: 中南工业大学地质系, 1994: 1~236. DUAN Jia-ruan, LIU Ji-shun, HU Xiang-zhao. Revision and description of 1:50000 geologic map and research of the metallogenic prediction in Dongchuan copper mining area, Yunnan Province[R]. Changsha:Department of Geology of Central South Technology University, 1994:1~236.
[2]	吴懋德, 段锦荪.云南昆阳群地质[M].昆明:云南科技出版社, 1990:1~200. WU Mao-de, DUAN Jin-sun.Geology of the Kunyang Group in Yunnan[M].Kunming:Yunnan Science and Technology Press, 1990:1~200.
[3]	花友仁.对东川铜矿地层的划分和区域构造的探讨[J].地质论评, 1959, 19(4):155~162. http://www.geojournals.cn/georev/ch/reader/view_abstract.aspx?file_no=19590449&flag=1 HUA You-ren. The division of strata of Dongchuan copper mine and regional tectonic discussed[J]. Geological Review, 1959, 19(4):155~162. http://www.geojournals.cn/georev/ch/reader/view_abstract.aspx?file_no=19590449&flag=1
[4]	黄仲权.昆阳群的滑覆构造的控矿作用[J].云南地质, 1997, 16(1):40~51. http://www.cnki.com.cn/Article/CJFDTOTAL-YNZD199701001.htm HUANG Zhong-quan. On the ore-control of slipping nappe in Kunyang Group[J]. Yunnan Geology, 1997, 16(1):40~51. http://www.cnki.com.cn/Article/CJFDTOTAL-YNZD199701001.htm
[5]	李希勣.建立康滇地轴区中-晚元古代层型剖面的雏议[J].云南地质, 1993, 12(1):101~108. http://www.cnki.com.cn/Article/CJFDTOTAL-YNZD199301015.htm LI Xi-ji. Preliminary discussion on establishment of middle and late proterozoic stratotype section in the Xikang-Yunnan axis region[J]. Yunnan Geology, 1993, 12(1):101~108. http://www.cnki.com.cn/Article/CJFDTOTAL-YNZD199301015.htm
[6]	李希勣.再论建立康滇地轴区中晚元古代层型剖面问题[J].云南地质, 1999, 18(1):89~91. http://www.cnki.com.cn/Article/CJFDTOTAL-YNZD901.009.htm LI Xi-ji. More discussion on establishment of middle and late proterozoic stratotype section in the Xikang-Yunnan axis region[J]. Yunnan Geology, 1999, 18(1):89~91. http://www.cnki.com.cn/Article/CJFDTOTAL-YNZD901.009.htm
[7]	李希勣, 吴懋德, 段锦荪.昆阳群的层序及顶底问题[J].地质论评, 1984, 30(5):399~408. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP198603009.htm LI Xi-ji, WU Mao-de, DUAN Jin-sun. The stratigraphic sequence of the Kunyang Group and its top and bottom boundaries[J]. Geological Review, 1984, 30(5):399~408. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP198603009.htm
[8]	陈天佑.东川矿区前寒武系昆阳群因民组下伏地层层位的探讨[J].西南矿产地质, 1989, 3(1):27~30. CHEN Tian-you. Discussion of the Precambrian underlying layers of the Yinmin formation of Kunyang group in Dongchuan region[J]. Mineral Geology of Southwest, 1989, 3(1):27~30.
[9]	王承尧.东川地区元古界地层划分的探讨[J].云南地质, 1987, 6(4):362~366. http://www.cnki.com.cn/Article/CJFDTOTAL-YNZD198704011.htm WANG Cheng~yao. Discussion of division of Proterozoic strata in Dongchuan region[J]. Yunnan Geology, 1987, 6(4):362~366. http://www.cnki.com.cn/Article/CJFDTOTAL-YNZD198704011.htm
[10]	刘肇昌.扬子地台西缘构造演化与金属成矿[M].成都:电子科技大学出版社, 1996:1~147. LIU Zhao-chang. Tectonic evolution and metal mineralization in the west margin of Yangtz platform[M]. Chengdu:University of Electronic Science and Technology of China Press, 1996:1~147.
[11]	李天福.东川矿区"小溜口组"地层特征及与因民组的接触关系[J].云南地质, 1993, 12(1):1~11. http://www.cnki.com.cn/Article/CJFDTOTAL-YNZD199301001.htm LI Tian-fu. Stratigraphic characteristics of "Xiaoliukou Formation" and its contact relation with Yinmin Formation in Dongchuan mining district[J]. Yunnan Geology, 1993, 12(1):1~11. http://www.cnki.com.cn/Article/CJFDTOTAL-YNZD199301001.htm
[12]	孙家骢.论昆阳群对比及划分[J].昆明工学院学报, 1982, (3):1~9. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=kmlg198301000&dbname=CJFD&dbcode=CJFQ SUN Jia-cong. On the division and correlation of Kunyang Group[J]. Journal of Kunming Engineering Institute, 1982, (3):1~9. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=kmlg198301000&dbname=CJFD&dbcode=CJFQ
[13]	桂林冶金地质研究所变质岩铜矿专题组.东川铜矿的地层岩石特征及其与成矿的关系[J].地质与勘探, 1975, (4):18~25. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKT197504003.htm Metamorphic Rocks Under Copper Mine Team of Guilin Metallurgy Geological Institute. Strata rock characteristics and metallogenic relationship of Dongchuan copper mine[J]. Geology and Prospecting, 1975, (4):18~25. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKT197504003.htm
[14]	潘杏南, 赵济湘, 张选阳, 等.康滇构造与裂谷作用[M].重庆:重庆出版社, 1987:11~133. PAN Xing-nan, ZHAO Ji-xiang, ZHANG Xuan-yang, et al. Xikang-Yunnan tectonics and riftogenesis[M]. Chongqing:Chongqing Publishing House, 1987:11~133.
[15]	牟传龙, 林仕良, 余谦.四川会理-会东及邻区中元古界昆阳群沉积特征及演化[J].沉积与特提斯地质, 2000, 20(1):44~51. http://www.cnki.com.cn/Article/CJFDTOTAL-TTSD200001002.htm MOU Chuan-long, LIN Shi-liang, YU Qian. Sedimentation and evolution of the Mesoproterozoic Kunyang Group in the Huili-Huidong region, Sichuan and its adjacent areas[J]. Sedimentary Geology and Tethyan Geology, 2000, 20(1):44~51. http://www.cnki.com.cn/Article/CJFDTOTAL-TTSD200001002.htm
[16]	尹福光, 孙志明, 白建科.东川、滇中地区中元古代地层格架[J].地层学杂志, 2011, 35(1):49~54. http://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ201101009.htm YIN Fu-guang, SUN Zhi-ming, BAI Jian-ke. Stratigraphic framework of the Mesoproterozoic in Dongchuan and central Yunnan region[J]. Journal of Stratigraphy, 2011, 35(1):49~54. http://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ201101009.htm
[17]	薛步高.因民组下限接触关系并对昆阳群层序的讨论[J].云南地质, 1987, 6(2):174~178. http://www.cnki.com.cn/Article/CJFDTOTAL-YNZD198702006.htm XUE Bu-gao. Discussion of contact with the lower limit of the Yinmin Formation and the Kunyang Group layers[J]. Yunnan Geology, 1987, 6(2):174~178. http://www.cnki.com.cn/Article/CJFDTOTAL-YNZD198702006.htm
[18]	戴恒贵.康滇地区昆阳群和会理群地层、构造及找矿靶区研究[J].云南地质, 1997, 16(1):1~39. http://www.cnki.com.cn/Article/CJFDTOTAL-YNZD199701000.htm DAI Heng-gui. On the strata, structure and prospecting target area of Kunyang Group and Huili Group in Kang-dian region[J]. Yunnan Geology, 1997, 16(1):1~39. http://www.cnki.com.cn/Article/CJFDTOTAL-YNZD199701000.htm
[19]	熊兴武, 候蜀光, 薛顺荣.滇中昆阳群因民角砾岩及其成因[J].地质科技情报, 1995, 14(4):43~48. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ504.010.htm XIONG Xing-wu, HOU Shu-guang, XUE Shun-rong. Yinmin breccia and its origin, proterozoic Kunyang Group, central Yunnan Province[J]. Geological Science and Technology Information, 1995, 14(4):43~48. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ504.010.htm
[20]	朱华平, 范文玉, 周邦国, 等.论东川地区前震旦系地层层序:来自锆石SHRIMP及LA-ICP-MS测年的证据[J].高校地质学报, 2011, 17(3):452~461. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX201103012.htm ZHU Hua-ping, FAN Wen-yu, ZHOU Bang-guo, et al. Assessing precambrian stratigraphic sequence of dongchuan area:evidence from zircon SHRIMP and LA-ICP-MS dating[J]. Geological Journal of China Universities, 2011, 17(3):452~461. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX201103012.htm