吉林大学学报(地球科学版) ›› 2019, Vol. 49 ›› Issue (3): 737-745.doi: 10.13278/j.cnki.jjuese.20180023

• 地质与资源 • 上一篇    下一篇

朝鲜平南盆地叠加褶皱构造特征

金炳成1,2, 刘永江3,4, 卞昌男5, 朴明华5   

  1. 1. 中国地质大学地球科学与资源学院, 北京 100083;
    2. 金策工业综合大学资源探测工程学院, 朝鲜 平壤 999162;
    3. 中国海洋大学海洋地球科学学院, 山东 青岛 266100;
    4. 吉林大学地球科学学院, 长春 130061;
    5. 平南综合大学煤炭工业学院, 朝鲜 平城 999093
  • 收稿日期:2018-01-30 出版日期:2019-06-03 发布日期:2019-06-03
  • 通讯作者: 刘永江(1964-),男,教授,博士生导师,主要从事构造地质学方面的研究,E-mail:yongjiang@jlu.edu.cn E-mail:yongjiang@jlu.edu.cn
  • 作者简介:金炳成(1972-),男,副教授,主要从事地层古生物与区域构造地质学方面的研究,E-mail:kbs1972@126.com
  • 基金资助:
    国家重点研发计划项目（2017YFC0601300-01）

Characteristics of Superposed Folds of Pyongnam Basin in Korean Peninsula

Kim Byongsong1,2, Liu Yongjiang3,4, Byon Changnam5, Pak Myonghwa5   

  1. 1. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China;
    2. College of Resources Exploration Engineering, Kim Chaek University of Technology, Pyongyang, 999162, Korea;
    3. College of Marine Geo-Sciences, Ocean University of China, Qingdao 266100, Shandong, China;
    4. College of Earth Sciences, Jilin University, Changchun 130061, China;
    5. College of Coal Industry, Pyongnam University, Pyongsong, 999093, Korea
  • Received:2018-01-30 Online:2019-06-03 Published:2019-06-03
  • Supported by:
    Supported by National Key R & D Basic Program of China(2017YFC0601300-01)

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摘要： 对于朝鲜平南盆地沉积盖层内发育的倒转褶皱，过去一般认为是直立褶皱的次级从属褶皱。通过对平南盆地内倒转褶皱发育区详细的地质调查，结合煤炭开发过程中获得的地质及钻探资料，提出平南盆地内叠加褶皱的主要识别标志为：地质平面图上呈现不同类型的两组褶皱脊线的交叉；倒转褶皱的轴面被直立褶皱改造弯曲；直立褶皱的两翼发育的倒转褶皱表现为两组牵引褶皱。查明了平南盆地存在3个阶段的褶皱构造：第一阶段为东西向的倒转褶皱，形成于印支期；第二阶段褶皱为东西向的直立褶皱，形成于早燕山期；第三阶段褶皱为北北东向的直立褶皱，形成于晚燕山期。

关键词: 平南盆地, 沉积盖层, 叠加褶皱, 倒转褶皱

Abstract: The inverted folds developed in the sedimentary cap rocks in the Pyongnam basin are generally considered to be subordinate folds of upright folds. According to the detailed investigation and the geological and drilling data obtained in the process of coal development, we think that the main recognition marks of the superposed folds in the basin are as follows:The intersection of two different ridge lines of fold on the geological plane map; The axial surface of inverted folds reformed by upright folds; The inverted folds that developed in the two limbs of upright folds and showed the nature of two groups of traction folds. There are three stages of folds identified in the Pyongnam basin:the first stage is the E-W trending inverted folds formed in Indosinian stage; the second stage is the E-W trending upright folds formed in Early Yanshanian stage; and the third stage is the NNE trending upright folds formed in Late Yanshanian stage.

Key words: Pyongnam basin, sedimentary cover, superposed folds, inverted folds

中图分类号: 

  • P548
[1] Gang Hyonggap. The Type of Fold Structures and Superposition[J]. Science of Geology and Geography, 1984,3:9-11. (in Korean)
[2] Geological Institute Academy of Science DPR of Korea. Geology of Korea[M]. Pyongyang:Foreign Languages Books Publishing House, 1993:26-48.
[3] 金炳成. 中国东部-朝鲜半岛古生代沉积特征及构造演化[D]. 长春:吉林大学, 2012:41-49. Kim Byongsong. Characteristics of Paleozoic Sedimentary from East China-Korean Peninsula and Its Tectonic Evolution[D]. Changchun:Jilin University, 2012:41-49.
[4] 刘志宏, 王芃, 刘永江, 等. 柴达木盆地南翼山-尖顶山地区构造特征及变形时间的确定[J]. 吉林大学学报(地球科学版), 2009, 39(5):796-802. Liu Zhihong, Wang Peng, Liu Yongjiang, et al. Structural Features and Determination of Deformation Time in the Nanyishan-Jiandingshan Area of Qaidam Basin[J]. Journal of Jilin University (Earth Science Edition), 2009, 39(5):796-802.
[5] 彭兆蒙, 彭仕宓, 吴智平, 等. 华北东部侏罗-白垩纪盆地演化及其对构造运动的响应[J]. 西安石油大学学报(自然科学版), 2009, 24(5):7-12. Peng Zhaomeng, Peng Shimi, Wu Zhiping, et al. Evolution of the Jurassic-Cretaceous Basins in the Eastern Part of North China and Its Response to the Tectonic Movement[J]. Journal of Xi'an Shiyou University (Natural Science Edition), 2009, 24(5):7-12.
[6] 张允平, 李景春. 华北及其以北地区晚古生代-早中生代构造格架主体特点[J]. 中国地质, 2010, 37(4):916-930. Zhang Yunping, Li Jingchun. Tectonic Framework and Main Characteristics of North China and Its Northward Areas in Late Paleozoic-Early Mesozoic Period[J]. Geology in China, 2010, 37(4):916-930.
[7] 骆满生, 卢隆桥, 贾建, 等. 中国中生代沉积盆地演化[J]. 地球科学:中国地质大学学报, 2014, 39(8):954-976. Luo Mansheng, Lu Longqiao, Jia Jian, et al. Evolution of Sedimentary Basins in China During Mesozoic[J]. Earth Science:Journal of China University of Geosciences, 2014, 39(8):954-976.
[8] 杨海斌, 田小波, 白志明, 等. 浅谈中国大陆东缘中生代地质演化与泛太平洋板块活动的关系[J]. 吉林大学学报(地球科学版), 2016,46(3):781-797. Yang Haibin, Tian Xiaobo, Bai Zhiming, et al. Discussion on the Relationship Between Pan Pacific Plate Movement and Mesozoic Geological Evolution of Eastern Chinese Continent[J]. Journal of Jilin University(Earth Science Edition), 2016,46(3):781-797.
[9] Byon Changnam, Pak Myonghwa. Study of Superposed Folds at the 00 Region[J]. Science of Geology and Geography, 2008,4:45-46.(in Korean)
[10] 马杏垣, 白瑾, 索书田, 等. 中国前寒武纪构造格架及研究方法[M]. 北京:地质出版社, 1987:31-33. Ma Xingyuan, Bai Jin, Suo Shutian, et al. Precambrian Tectonic Framework and Research Methods in China[M]. Beijing:Geological Publishing House, 1987:31-33.
[11] Ramsay J G, Huber M I. The Techniques of Modern Structural Geology, Vol 2:Folds and Fractures[M]. London:Academic Press, 1987:475-501.
[12] 陈龙, 施炜. 叠加褶皱研究进展综述[J]. 地质力学学报, 2014, 20(4):455-468. Chen Long, Shi Wei. Superposed Fold:An Overview[J]. Journal of Geomechanics, 2014, 20(4):455-468.
[13] Shi Wei, Dong Shuwen, Zhang Yueqiao, et al. The Typical Large-Scale Superposed Folds in the Central South China:Implications for Mesozoic Intracontinental Deformation of the South China Block[J]. Tectonophysics, 2015, 664:50-66.
[14] Byon Changnam, Kim Byongsong. Distribuion of Primary Chinley Coal in Dokchon-Bukchang Region[J]. Geological Survey, 2005,5:22-25.(in Korean)
[15] Kim Byongsong, Byon Changnam. Characteristics and Formation Causes of Fold Structure Developed to the East of Chang'an Mountain Syncile[J]. Academy of Sciences Bulletin, 2011,1:40-42.(in Korean)
[16] 王桂梁. 论中国煤矿中的叠加褶皱[J]. 地学前缘, 1999, 6(增刊):175-182. Wang Guiliang. Discussion on Superposed Folds in Coal Mines of China[J]. Earth Science Forntiers, 1999, 6(Sup.):175-182.
[17] 崔盛芹, 李锦蓉. 试论中国滨太平洋带的印支运动[J]. 地质学报, 1983, 57(1):51-61. Cui Shengqin, Li Jinrong. A Discussion Margin-Pacific Indosian Movement in China[J].Acta Geologica Sinica, 1983, 57(1):51-61.
[18] Bartolini A, Larson R L. Pacific Microplate and the Pangea Supercontinent in the Early to Middle Jurassic[J]. Geology, 2001, 29(8):735-738.
[19] 刘正宏, 徐仲元. 阴山地区印支期地壳构造变形研究[J]. 吉林大学学报(地球科学版), 2003, 33(1):1-6. Liu Zhenghong, Xu Zhongyuan. Research of Indosinian Crust Structural Deformation at Yinshan Area[J]. Journal of Jilin University(Earth Science Edition), 2003, 33(1):1-6.
[20] 张允平. 东北亚地区晚侏罗世-白垩纪构造格架主体特点[J]. 吉林大学学报(地球科学版), 2011,41(5):1267-1284. Zhang Yunping. Main Characteristics of Late Jurassic-Cretaceous Tectonic Framework in Northeast Asia[J]. Journal of Jilin University(Earth Science Edition), 2011,41(5):1267-1284.
[21] 葛肖虹, 马文璞, 刘俊来, 等. 对中国大陆构造格架的讨论[J].中国地质, 2009, 36(5):949-965. Ge Xiaohong, Ma Wenpu, Liu Junlai, et al. A Discussion on the Tectonic Framework of Chinese Mainland[J]. Geology in China, 2009, 36(5):949-965.
[22] 唐贤君, 於文辉, 单蕊. 中国东部-朝鲜半岛中生代板块结合带划分研究现状与问题[J]. 地质学报, 2010,84(5):606-617. Tang Xianjun, Yu Wenhui, Shan Rui. The Mesozoic Plate Boundary in the Eastern China and Korean Peninsula:Present Studies and Problems[J]. Acta Geologica Sinica, 2010,84(5):606-617.
[23] Oh Changwhan. A New Concept on Tectonic Correlation Between Korea, China and Japan:Histories from the Late Proterozoic to Cretaceous[J]. Gondwana Research, 2006, 9(1/2):47-61.
[24] Zhai Mingguo, Guo Jinghui, Li Zhong, et al. Linking the Sulu UHP Belt to the Korean Peninsula:Evidence from Eclogite, Precambrian Basement, and Paleozoic Sedimentary Basins[J]. Gondwana Research, 2007, 12(4):388-403.
[25] Sajeev K, Jeong Jaehoon, Kwon Sanghoon, et al. High p-t Granulite Relicts from the Imjingang Belt, South Korea:Tectonic Significance[J]. Gondwana Research, 2010, 17(1):75-86.
[26] 武昱东, 侯泉林. 大别-苏鲁造山带在朝鲜半岛的延伸方式:基于40Ar/39Ar构造年代学的约束[J]. 岩石学报, 2016, 32(10):3187-3204. Wu Yudong, Hou Quanlin. The Extension of the Dabie-Sulu Orogenic Belt in Korean Peninsula:Based on 40Ar/39Ar Tectonic Chronology[J]. Acta Petrologica Sinica, 2016, 32(10):3187-3204.
[27] 翟明国. 朝鲜半岛与华北地质之对比研究:进展与问题[J]. 岩石学报2016, 32(10):2915-2932. Zhai Mingguo. Comparative Study of Geology in North China and Korean Peninsula:Research Advances and Key Issues[J]. Acta Petrologica Sinica, 2016, 32(10):2915-2932.
[28] Chough S K, Kwon S T, Ree J H, et al. Tectonic and Sedimentary Evolution of the Korean Peninsula:A Review and New View[J]. Earth-Science Reviews, 2000,52:175-235.
[29] Kwon Y K, Chough S K, Choi D K, et al. Sequence Stratigraphy of the Taebaek Group (Cambrian-Ordovician), Mideast Korea[J]. Sedimentary Geology, 2006, 192(1/2):19-55.
[30] Niu Yaoling, Liu Yi, Xue Qiqi, et al. Exotic Origin of the Chinese Continental Shelf:New Insights Into the Tectonic Evolution of the Western Pacific and Eastern China Sincethe Mesozoic[J]. Science Bulletin, 2015, 60(18):1598-1616.
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