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
金炳成1,2, 刘永江3,4, 卞昌男5, 朴明华5
Kim Byongsong1,2, Liu Yongjiang3,4, Byon Changnam5, Pak Myonghwa5
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。
中图分类号:
[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. |
[1] | 金炳成, 刘永江, 杨卫民. 朝鲜平南盆地泥盆纪化石的发现及其地质意义[J]. J4, 2011, 41(1): 79-85. |
|