吉林大学学报(地球科学版) ›› 2015, Vol. 45 ›› Issue (2): 349-363.doi: 10.13278/j.cnki.jjuese.201502102
郑常青, 李娟, 金巍, 周建波, 施璐, 崔芳华, 韩晓萌
Zheng Changqing, Li Juan, Jin Wei, Zhou Jianbo, Shi Lu, Cui Fanghua, Han Xiaomeng
摘要:
松辽盆地西缘发育大型的北北东走向韧性断裂带,该韧性断裂带的性质、活动时限一直存在争议,制约了对松辽盆地构造成因的认识以及松辽盆地西缘油气勘探开发的进展。腾克、金星及嘎拉山地区是松辽盆地西缘韧性断裂带的代表性出露区,主体岩石组合为条带状花岗质糜棱岩、眼球状花岗质糜棱岩等。腾克、金星及嘎拉山地区发育一组糜棱面理和线理,其中面理为110°~135°∠45°~65°、线理为倾伏向10°~25°,倾伏角10°~35°;其运动性质均显示左行走滑特征。确定韧性断裂带活动时限的样品采自构造带内花岗质糜棱岩的锆石和同变形云母,其中锆石SHRIMP谐和年龄为296.9~299.4 Ma;黑云母40Ar-39Ar年龄为(123.0±0.7)Ma,白云母的40Ar-39Ar年龄为(124.4±0.9)Ma。松辽盆地西缘韧性断裂带应该属于嫩江断裂带的北段。年龄结果表明该韧性断裂带中花岗岩侵位于晚石炭世,大型北北东向韧性构造变形发生于早白垩世。腾克金星嘎拉山剪切带控制松辽盆地西缘,同时表明松辽盆地在早白垩世经历了走滑挤压盆地演化阶段,这种大型北北东向韧性断裂带的形成可能与当时西太平洋伊泽纳崎板块向欧亚大陆俯冲发生转向有关。
中图分类号:
[1] 黑龙江省地质矿产局. 黑龙江省区域地质志[M]. 北京: 地质出版社, 1993. Bureau of Geology and Mineral Resources of Heilongjiang Province. Regional Geology of Heilongjiang Province[M]. Beijing: Geological Publishing House, 1993.[2] 吉林省地质矿产局. 吉林省区域地质志[M]. 北京: 地质出版社, 1989. Bureau of Geology and Mineral Resources of Jilin Province. Regional Geology of Jilin Province[M]. Beijing: Geological Publishing House, 1989.[3] 内蒙古自治区地质矿产局. 内蒙古自治区区域地质志[M]. 北京: 地质出版社, 1991. Bureau of Geology and Mineral Resources of Inner Mongolia Autonomous Region. Regional Geology of Inner Mongolia Autonomous Region[M]. Beijing: Geological Publishing House, 1991.[4] 王荃, 刘雪亚, 李锦轶. 中国华夏与安哥拉古陆间的板块构造[M]. 北京: 北京大学出版社, 1991:122-134. Wang Quan, Liu Xueya, Li Jinyi. Plate Tectonics Between Cathaysia and Angaraland in China[M]. Beijing: Peking University Press, 1991: 122-134.[5] 黄汲清, 任纪舜. 关于大地构造研究的几个重要问题:构造地质学进展[M]. 北京: 科学出版社, 1982. Huang Jiqing, Ren Jishun. Several Important Problems of the Tectonic Research:Progress of Structural Geology[M]. Beijing: Science Press, 1982.[6] 张梅生, 彭向东, 孙晓猛. 中国东北区古生代构造古地理格局[J]. 辽宁地质, 1998(2): 91-96. Zhang Meisheng, Peng Xiangdong, Sun Xiaomeng. The Paleozoic Tectonic Geographicalopattern of Northeast China[J]. Liaoning Geology, 1998(2): 91-96.[7] 郭孟习, 孙炜, 尹国义, 等. 郯庐断裂系的北延及地质-地球物理特征[J]. 吉林地质, 2000, 19(3): 35-44. Guo Mengxi, Sun Wei, Yin Guoyi, et al. North-extension of the Tanlu Fracture and Geologic-Geophysical Characterisitics[J]. Jilin Geology, 2000, 19(3): 35-44.[8] 陈洪洲, 余中元, 许晓艳, 等. 嫩江断裂构造及其与地震活动的关系[J]. 东北地震研究, 2004, 20(4): 43-49. Chen Hongzhou, Yu Zhongyuan, Xu Xiaoyan, et al. Characteristics of Nenjiang Fracture Structure and the Relation Between This Fracture and Earthquake Activity[J]. Seismological Research of Northeast China, 2004, 20(4): 43-49.[9] 林存东, 戴昕志, 李贵明, 等. 嫩江断裂带地震活动特征分析[J]. 地震地磁观测与研究, 2005, 26(4): 18-21. Lin Cundong, Dai Xinzhi, Li Guiming, et al. Analysis of the Earthquake Activity Characterisitics Around the Nenjiang Fracture Belt[J]. Seismological and Geomagnetic Observation and Reserch, 2005, 26(4): 18-21.[10] 傅维洲, 贺日政. 松辽盆地及周边地带地震构造特征[J]. 世界地质, 1999, 18(2): 95-100. Fu Weizhou, He Rizheng. Structural Characteristics of Earthquakes in Songliao Basin and Its Peripheral Regions[J].World Geology, 1999, 18(2): 95-100.[11] Wang Yufang, Zheng Yadong, Zang Qijia, et al.Glassy Matrix of Pseudotachylite in the Yagan Extensional Detachment Fault in the Sino-Mongolian Boundary and Its Kinematic Implications[J]. Chinese Science Bulletin, 1994, 22(39): 1895-1899.[12] Han Baofu, Zheng Yadong, Gan Jiangwu. The Luozidian Normal Fault Near Chifeng, Inner Mongolia: Master Fault of a Quasi-Metamorphic Core Complex[J]. International Geology, 2001, 3(43): 254-264.[13] 张晓晖, 李铁胜, 蒲志平, 等. 内蒙古赤峰娄子店大城子韧性剪切带的40Ar-39Ar年龄及其构造意义[J]. 科学通报, 2002, 47(12): 951-956. Zhang Xiaohui, Li Tiesheng, Pu Zhiping, et al.40Ar-39Ar Ages of Louzidian-Dachengzi Ductile Shear Zone in Chifeng, Inner Mongolia and Its Tectonic Significance[J]. Chinese Science Bulletin, 2002, 47(12): 951-956.[14] 杨承先, 王贵华, 陈健. 内蒙红山八里罕断裂地质特征及其地震活动性[J]. 地震研究, 1984, 4(7): 391-398. Yang Chengxian, Wang Guihua, Chen Jian. The Hongshan-Balihan Fault Zone, Inner Mongolia-Its Geologic Features and Seismicity[J]. Journal of Seismological Research, 1984, 4(7): 391-398.[15] 王新社, 郑亚东. 楼子店变质核杂岩韧性变形作用的40Ar/39Ar年代学约束[J]. 地质论评, 2005, 51(5): 574-582. Wang Xinshe, Zheng Yadong.40Ar/39Ar Age Constraints on the Ductile Deformation of the Detachment System of the Louzidian Core Complex, Southern Chifeng, China[J]. Geological Review, 2005, 51(5): 574-582.[16] 刘伟, 杨进辉, 李潮峰. 内蒙赤峰地区若干主干断裂带的构造热年代学[J]. 岩石学报, 2003, 19(4): 717-728. Liu Wei, Yang Jinhui, Li Chaofeng.Thermochronology of Three Major Faults in the Chifeng Area, Inner Mongolia of Chian[J]. Acta Petrologica Sinica, 2003, 19(4): 717-728.[17] Zhou Jianbo, Simon A W, Zhao Guochun, et al. Pan-African Metamorphic and Magmatic Rocks of the Khanka Massif, NE China: Further Evidence Regarding Their Affinity[J]. Geological Magazine, 2010, 147(5): 737-749.[18] Zhou Jianbo, Simon A W. The Crustal Accretion History and Tectonic Evolution of the NE China Segment of the Central Asian Orogenic Belt[J]. Gondwana Research, 2013, 23(4): 1365.[19] Wu Fuyuan, Zhao Guochun, Sun Deyou, et al. The Hulan Group: Its Role in the Evolution of the Central Asian Orogenic Belt of NE China[J]. Journal of Asian Earth Sciences, 2007, 30(3): 542-556.[20] Simon A W, Zhang Xingzhou, Wu Fuyuan. Extension of a Newly-Identified 500 Ma Metamorphic Terrain in Northeast China: Further U-Pb SHRIMP Dating of the Mashan Complex, Heilongjiang Province, China[J]. Tectonophysics, 2000(328): 115-130.[21] 郑常青, 周建波, 金巍, 等. 大兴安岭地区德尔布干断裂带北段构造年代学研究[J]. 岩石学报, 2009, 25(8): 1989-2000. Zheng Changqing, Zhou Jianbo, Jin Wei, et al. Geochronology in the North Segment of the Derbugan Fault Zone, Great Xing'an Range, NE China[J].Acta Petrologica Sinica, 2009, 25(8): 1989-2000.[22] Zhou Jianbo, Simon A W, Zhao Guochun, et al. SHRIMP U-Pb Zircon Dating of the Neoproterozoic Penglai Group and Archean Gneisses from the Jiaobei Terrane, North China, and Their Tectonic Implications[J]. Precambrian Research, 2008(160): 323-340.[23] Zhou Jianbo, Simon A W, Zhao Guochun, et al. SHRIMP U-Pb Zircon Dating of the Wulian Complex: Defining the Boundary Between the North and South China Cratons in the Sulu Orogenic Belt, China[J]. Precambrian Research, 2008(162): 559-576.[24] Zhou Jianbo, Simon A W, Zhao Guochun, et al. Detrial Zircon U-Pb Dating of Low-Grade Metamorphic Rocks in the Sulu UHP Belt: Evidence for Overthrusting of the North China Block Above the South China Block During Continental Subduction[J]. Journal of Geological Society, 2008(165): 423-433.[25] 刘树文, 吕勇军, 凤永刚, 等. 冀北单塔子杂岩的地质学和锆石U-Pb年代学[J]. 高校地质学报, 2007(3): 484-497. Liu Shuwen, Lü Yongjun, Feng Yonggang, et al. Geology and Zircon U-Pb Isotopic Chronology of Dantazi Complex, Norhern Hebei Province[J]. Geological Journal of China Universities, 2007(3): 484-497.[26] Wan Yusheng, Li Renwei, Simon A W, et al. UHP Metamorphism and Exhumation of the Dabie Orogen, China: Evidence from SHRIMP Dating of Zircon and Monazite from a UHP Granitic Gneiss Cobble from the Hefei Basin[J]. Geochimica Et Cosmochimica Acta, 2005(69): 4333-4348.[27] Liu Fulai, Xu Zhiqin, Xue Huaimin. Tracing the Protolith, UHP Metamorphism, and Exhumation Ages of Orthogneiss from the SW Sulu Terreane (Eastern China):SHRIMP U-Pb Dating of Mineral Inclusion Bearing Zircons[J]. Lithos, 2004(78): 411-429.[28] Kenneth R L. Users Manual for Isoplot/Ex (rev. 2.49): A Geochronological Toolkit for Microsoft Excel[M]. Berkeley: Special Publication, 2001: 1-55.[29] Simon A W, John W V, William H P, et al. Evidence from Detrital Zircons for the Existence of Continental Crust and Oceans on the Earth 4.4 Gyr Ago[J]. Nature, 2001, 409: 175-178.[30] 闫全人, 王宗起, 闫臻, 等. 构造变形/变质作用的精细测年及其在造山带研究中的应用[J]. 地学前缘, 2001, 8(3): 147-156. Yan Quanren, Wang Zongqi, Yan Zhen, et al. Detailed Dating of Deformation/Metamorphism of Shear Zones on the Scale of Orogen and Its Application[J]. Earth Science Frontiers, 2001, 8(3): 147-156.[31] 赵芝. 大兴安岭北部晚古生代岩浆作用及其构造意义[D]. 长春:吉林大学, 2011. Zhao Zhi. Late Paleozoic Magmatism and Its Tectonic Significance in the Northern Great Xing'an Range, Northeastern China[D].Changchun: Jilin University, 2011.[32] 赵芝, 迟效国, 潘世语, 等. 小兴安岭西北部石炭纪地层火山岩的锆石LA-ICP-MS U-Pb年代学及其地质意义[J]. 岩石学报, 2010, 26(8): 2452-2464. Zhao Zhi, Chi Xiaoguo, Pan Shiyu, et al. Zircon U-Pb LA-ICP-MS Dating of Carboniferous Volcanics and Its Geological Significance in the Norhwestern Lesser Xing'an Range[J]. Acta Petrologica Sinica, 2010, 26(8): 2452-2464.[33] 葛文春, 吴福元, 周长勇, 等. 大兴安岭中部乌兰浩特地区中生代花岗岩的锆石U-Pb年龄及地质意义[J]. 岩石学报. 2005, 21(3): 749-762. Ge Wenchun, Wu Fuyuan, Zhou Changyong, et al. Zircon U-Pb Ages and Its Significance of the Mesozoic Granites in the Wulanhaote Region, central Da Hinggan Mountain[J]. Acta Petrologica Sinica, 2005, 21(3): 749-762.[34] 柳长峰, 杨帅师, 武将伟, 等. 内蒙古中部四子王旗地区晚二叠早三叠世过铝花岗岩定年及成因[J]. 地质学报, 2010, 21(7): 1002-1016. Liu Changfeng, Yang Shuaishi, Wu Jiangwei, et al. Dating and Petrogenesis of Late Permian-Early Triassic Peraluminous Granites in the Siziwangqi Area, Inner Mongolia[J]. Acta Geologica Sinica, 2010, 21(7): 1002-1016.[35] 石玉若, 刘敦一, 张旗, 等. 内蒙古中部苏尼特左旗地区三叠纪A型花岗岩锆石SHRIMP U-Pb年龄及其区域构造意义[J]. 地质通报, 2007, 26(2): 183-189. Shi Yuruo, Liu Dunyi, Zhang Qi, et al. SHRIMP U-Pb Zircon Dating of Triassic A-Type Granites in Sonid Zuoqi, Central Inner Mongolia, China and Its Tectonic Implications[J]. Geological Bulletin of China, 2007, 26(2): 183-189.[36] 张连昌, 英基丰, 陈志广, 等. 大兴安岭南段三叠纪基性火山岩时代与构造环境[J]. 岩石学报, 2008, 24(4): 911-920. Zhang Lianchang, Ying Jifeng, Chen Zhiguang, et al. Age and Tectonic Setting of Triassic Basic Volcanic Rocks in Southern Da Hinggan Range[J]. Acta Petrologica Sinica, 2008, 24(4): 911-920.[37] 张万益, 聂凤军, 高延光, 等. 内蒙古查干敖包三叠纪碱性石英闪长岩的地球化学特征及成因[J]. 岩石学报, 2012, 28(2): 525-534. Zhang Wanyi, Nie Fengjun, Gao Yanguang, et al.Geochemical Characteristics and Genesis of Triassic Chagan Obo Alkaline Quartz Diorites in Inner Mongolia[J]. Acta Petrologica Sinica, 2012, 28(2): 525-534.[38] 张维, 简平, 刘敦一, 等. 内蒙古中部达茂旗地区三叠纪花岗岩和钾玄岩的地球化学、年代学和Hf同位素特征[J]. 地质通报, 2010, 29(7): 821-832. Zhang Wei, Jian Ping, Liu Dunyi, et al. Geochemistry, Geochronology and Hf Isotopic Compositions of Triassic Granodioritediorite and Shoshonite from the Damaoqi Area, Central Inner Mongolia, China[J]. Geological Bulletin of China, 2010, 29(7):821-832.[39] 周漪, 葛文春, 王清海. 大兴安岭中部乌兰浩特地区中生代花岗岩的成因: 地球化学及Sr-Nd-Hf同位素制约[J]. 岩石矿物学杂志. 2011, 30(5): 901-923. Zhou Yi, Ge Wenchun, Wang Qinghai. Petrogenesis of Mesozoic Granite in Wulanhaote Region, Central Da Hinggan Mountains: Constraints from Geoche-mistry and Sr-Nd-Hf Isotope[J]. Acta Petrologica Et Mineralogica, 2011, 30(5): 901-923.[40] 徐久磊, 郑常青, 施璐, 等. 大兴安岭北段雅尔根楚Ⅰ型花岗岩年代学、岩石地球化学及其地球动力学意义[J]. 地质学报, 2013, 87(9): 1311-1323. Xu Jiulei, Zheng Changqing, Shi Lu, et al. Geochronology and Geochemistry of the Yaergenchu I Type Granites in Northern Da Hinggan Range and Its Geodynamic Implications[J]. Acta Geologica Sinica, 2013, 87(9): 1311-1323.[41] Maruyama S, Isozaki Y, Kimura G, et al. Paleogeographic Maps of the JapaneseIslands: Plate Tectonic Synthesis from 750 Ma to the Present[J]. The Island Arc, 1997, 6: 121-142.[42] Engebretson D C, Thompson G A, Cox A. Correlation of Plate Motions with Continental Tectonics: Laramide to Basin-Range[J]. Tectonics, 1984, 3(2): 115-119.[43] Maruyama S, Send T. Orogeny and Relative Plate Motions: Example of the Japanese Islands[J]. Tectonophysics, 1986, 127(3/4): 305-329.[44] Deino A L, Orsi G, De Vita S, et al. The Age of the Neapolitan Yellow Tuff Caldera-Forming Eruption (Campi Flegrei Caldera-Italy) Assessed by 40Ar/39Ar Dating Method[J]. Journal of Volcanology and Geothermal Research, 2004, 133(1/2/3/4): 157-170.[45] 关德范. 松辽盆地的形成与发展[J]. 大庆石油学院学报, 1981(4): 1-10. Guan Defan. The Formation and Development of Songliao Basin[J]. Journal of Daqing Petroleum Institute, 1981(4): 1-10.[46] 李娟, 舒良树. 松辽盆地中、新生代构造特征及其演化[J]. 南京大学学报:自然科学版, 2002, 38(4): 525-531. Li Juan, Shu Liangshu. Mesozoic-Cenozoic Tectonic Features and Evolution of the Songliao Basin, NE China[J]. Journal of Nanjing University:Natural Sciences, 2002, 38(4): 525-531.[47] 刘福春, 程日辉, 解启来, 等. 松辽盆地梨树断陷页岩气资源潜力评价[J]. 吉林大学学报:地球科学版, 2014, 44 (3): 762-773. Liu Fuchun, Cheng Rihui, Xie Qilai, et al. The Potential Evaluation of Shale Gas Resources of Lishu Fault Depression in Songliao Basin[J]. Journal of Jilin University:Earth Science Edition, 2014, 44 (3): 762-773.[48] 朱光, 王道轩, 刘国生, 等. 郯庐断裂带的演化及其对西太平洋板块运动的响应[J]. 地质科学, 2004, 39(1): 36-49. Zhu Guang, Wang Daoxuan, Liu Guosheng, et al. Evolution of the Tan-Lu Fault Zone and Its Responses to Plate Movements West Pacific Basin[J]. Chinese Journal of Geology, 2004, 39(1): 36-49.[49] 张兴洲, 马玉霞, 迟效国, 等. 东北及内蒙古东部地区显生宙构造演化的有关问题[J]. 吉林大学学报:地球科学版, 2012, 42(5): 1269-1285. Zhang Xingzhou, Ma Yuxia, Chi Xiaoguo, et al. Discussion on Phanerozoic Tectonic Evolution in Nor-theastern China[J]. Journal of Jilin University:Earth Science Edition, 2012, 42(5): 1269-1285. |
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