朝鲜半岛古生代中期—中生代早期构造格局
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摘要
古生代中期─中生代早期朝鲜半岛发生了两次主要构造事件,即古生代中期朝鲜半岛中部临津江构造带的活动和古生代晚期—中生代早期朝鲜半岛北部豆满江造山带(咸北地块)的碰撞拼接事件。临津江带的地层、化石和构造等特征研究表明临津江带形成于志留纪末—泥盆纪初,结束于中生代三叠纪松林期;根据咸北地块沉积地层的岩浆岩岩石学、年代学资料,认为豆满江造山带的碰撞拼接时期可能是二叠纪—三叠纪。黄海地球物理、地震研究,朝鲜半岛大地构造和沉积盖层研究结果表明苏-鲁高压变质带没有延伸到临津江带,而是被近南北向纵贯朝鲜西海的断裂右行错移到了济洲岛以南;咸北地块和输城川断裂带的地质特征研究表明,咸北地块可能与佳木斯地块相连接,输城川断裂带可能与牡丹江断裂带相连接。
There are two main tectonic events in Korean Peninsula in Middle Paleozoic——Early Mesozoic,that are the activity of Limjingang belt in middle Korean Peninsula in Middle Paleozoic and the collision event of Domangang orogenic belt(Hambuk Masiff) in the northern part of Korean Peninsula in Late Paleozoic——Early Mesozoic.The research on the characteristics of strata,fossils and structure shows Limjingang belt formed in Late Silurian——Early Devonian,and ended in Songlin Stage of Triassic in Mesozoic.Based on the petrological and chronological data of sedimentary strata and magmatic rocks of Hambuk massif,it is considered that Domangang orogenic belt was formed during Permian——Trassic.The studies of geophysics and earthquake in the Yellow Sea and geotectonic and sedimentary strata show that Sulu high——pressure metamorphic belt not extended to Limjingang belt,but moved to the south of Cheju-do by the dextral fracture which north-south trending running across Korean West Sea.The study of geological characteristics in Hambuk massif and Susengchen fault zone show that Hambuk massif is probably connected with Jiamusi massif and Susengchen fault zone is probably connected with Mudanjiang fault zone.
There are two main tectonic events in Korean Peninsula in Middle Paleozoic——Early Mesozoic,that are the activity of Limjingang belt in middle Korean Peninsula in Middle Paleozoic and the collision event of Domangang orogenic belt(Hambuk Masiff) in the northern part of Korean Peninsula in Late Paleozoic——Early Mesozoic.The research on the characteristics of strata,fossils and structure shows Limjingang belt formed in Late Silurian——Early Devonian,and ended in Songlin Stage of Triassic in Mesozoic.Based on the petrological and chronological data of sedimentary strata and magmatic rocks of Hambuk massif,it is considered that Domangang orogenic belt was formed during Permian——Trassic.The studies of geophysics and earthquake in the Yellow Sea and geotectonic and sedimentary strata show that Sulu high——pressure metamorphic belt not extended to Limjingang belt,but moved to the south of Cheju-do by the dextral fracture which north-south trending running across Korean West Sea.The study of geological characteristics in Hambuk massif and Susengchen fault zone show that Hambuk massif is probably connected with Jiamusi massif and Susengchen fault zone is probably connected with Mudanjiang fault zone.
引文
①SHNG Gun Ho.朝鲜半岛地震带分布特征:博士论文[D].朝鲜平壤:地质研究所.2002.
[1]梁道俊,宋材秀.大地构造学[M].平壤:金日成综合大学出版社,2007:171-250.LYANG To Jun,Song Jae Su.Geotectonic geology[M].Pyongyang:Kim Il Sung University Press,2007:171-250.
[2]白龙浚.朝鲜地质[M].平壤:科学出版社,1998:1-160.BAEK Lyong Jun.Geology of Korea[M].Pyongyang:Science Press,1998:1-160.
[3]李炳柱.1∶250 000 Seoul-Namchonjeom地质图幅说明书[M].大田:韩国地质资源研究院,1999:1-64.LEE Byung Joo.Explanatory note of the 1∶250 000 Seoul-Namchonjeom sheet[M].Taejon:Korea Institute of Ge-ology,Mining and Materials,1999:1-64.
[4]李春昱.对亚洲地质构造发展的新认识[M].北京:科学出版社,1981:1-21.LI Chun-yu.Newideas of the tectonic development of A-sia[M].Beijing:Science Press,1981:1-21.
[5]任纪舜,王作勋.从全球看中国大地构造—中国及其邻区大地构造图简要说明[M].北京:地质出版社,1997:9-18.REN Ji-shun,WANG Zuo-xun.Tectonic of China asviewed over the globe—brief explanatory notes on the tec-tonic map of China and adjacent regions[M].Beijing:Geological Publishing House,1997:9-18.
[6]刘光鼎.中国海区及邻域地球物理场特征[M].北京:科学出版社,1992:1-150.LIU Guang-ding.Geophysical field features of China seaand adjacent regions[M].Beijing:Science Press,1992:1-150.
[7]Yin A,Nie S.An indentation mode for the North andSouth China collision and the development of the Tanluand Honamfaul systems,eastern Asia[J].Tectonics,1993,12:801-813.
[8]HAO Tian-yao,LIU Yi-ke,DUAN Chang.Characteris-tics of geophysical field in East China and adjacent re-gions[J].Geoscience Journal,1998,2(3):108-116.
[9]Suh Mancheol.Seismic stratigraphy of Henksan Basin inthe South Yellow Sea[C]//Suh Mancheol.Geologicalresources of the YellowSea.Kongju:Kongju National U-niversity,KOSEF,NSFC.1998:95-121.
[10]郝天珧,Suh Mancheol,王谦身,等.根据重力数据研究黄海周边断裂带在海区的延伸[J].地球物理学报,2002,45(3):385-398.HAO Tian-yao,Suh Mancheol,WANG Qian-shen,etal.The study of extension of faults in Yellow Sea andadjacent region from gravity data[J].Chinese Journalof Geophysics,2002,45(3):385-398.
[11]蔡乾忠.黄海含油气盆地区域地质与大地构造环境[J].海洋地质动态,2002,18(11):8-12.CAI Qian-zhong.Regional geology and geotectonic envi-ronment of petroliferous basins in the Yellow Sea[J].Marine Geology Letters,2002,18(11):8-12.
[12]戴明刚.黄海地质与地球物理特征研究进展[J].地球物理学进展,2003,18(3):583-591.DAI Ming-gang.Research progress in geology and geo-physics characters of the Yellow Sea[J].Progress inGeophysics,2003,18(4):583-591.
[13]郝天珧,刘建华,Suh Mancheol,等.黄海及邻区深部结构特点与地质演化[J].地球物理学报,2003,46(6):803-808.HAO Tian-yao,LIU Jian-hua,Suh Mancheol,et al.Deep structure characteristics and geological evolution inYellow Sea and adjacent region[J].Chinese Journal ofGeophysics,2003,46(6):803-808.
[14]郝天珧,Suh Mancheol,刘建华,等.黄海深部结构与中朝—扬子块体结合带在海区位置的地球物理研究[J].地学前缘,2004,11(3):51-61.HAO Tian-yao,Suh Mancheol,LIU Jian-hua,et al.Deep structure and boundary belt position between Sino-Korean and Yangtze blocks in Yellow Sea[J].EarthScience Frontiers,2004,11(3):51-61.
[15]葛肖虹,马文璞.东北亚南区中、新生代大地构造轮廓[J].中国地质,2007,34(2):212,222.GE Xiao-hong,MA Wen-pu.Mesozoic--Cenozoic frame-work of the southern Northeast Asia[J].Geology inChina,2007,34(2):212,222.
[16]秦蕴珊,赵一阳,陈丽蓉,等.黄海地质[M].北京:海洋出版社,1989:1-100.QIN Yun-shan,ZHAO Yi-yang,CHEN Li-rong,et al.Geology of Yellow Sea[M].Beijing:China OceanPress,1989:1-100.
[17]张文佑.中国海区及邻域海陆大地构造[M].北京:科学出版社,1986:575.ZHANG Wen-you.Marine and continental tectonics inChina seas and adjacent regions[M].Beijing:SciencePress,1986:575.
[18]杨志坚.胶东地块构造演化及其东延去向问题[J].海洋地质与第四纪地质,1989,9(2):1-11.YANG Zhi-jian.On the tectonic evolution of Jiaodongmassif and its extension to east[J].Marine Geologyand Quaternary Geology,1989,9(2):1-11.
[19]万天丰.中朝与扬子板块的鉴别特征[J].地质论评,2001,47(1):57-63.WAN Tian-feng.Distinctive characteristics of Sino-Ko-rean and Yangtze plates[J].Geological Review,2001,47(1):57-63.
[20]王谦身,安玉林.南黄海西部及邻域重力场与深部构造[J].科学通报,1999,44(22):2248-2453.WANG Qian-shen,AN Yu-lin.Gravity field and deepstructure in the western part of South YellowSea and ad-jacent area[J].Chinese Science Bulletion,1999,44(22):2448-2453.
[21]郝天珧,刘伊克,段昶.根据重磁资料探讨中国东部及其邻域断裂体系[J].地球物理学报,1996,39(增刊):141-149.HAO Tian-yao,LIUYi-ke,DUAN Chang.Approachingfault system of the East China and adjacent area fromgravity and magnetic data[J].Chinese Journal of Geo-physics,1996,39(Suppl.):141-149.
[22]蔡峰.北黄海盆地基底地质特征[J].海洋地质动态,1996,12(169):1-3.CAI Feng.Geological feature of the basement in theNorth Yellow Sea Basin[J].Marine Geology Letters,1996,12(169):1-3.
[23]陶宝国.南黄海周缘地区的地质构造联系[J].海洋地质译丛,1999,85(4):1-14.TAO Bao-guo.Relationship of geological tectonics a-round South Yellow Sea[J].Translation Collection ofMarine Geological,1999,85(4):1-14.
[24]CONG Bo-lin,ZHAI Ming-guo,Dennis C A,et al.Petrogenesis of ultrahigh-pressure rocks and their coun-try rock at Shuanghe in Dabieshan,central China[J].Eur J Mineral,1995,7:119-138.
[25]WANG Qing-chen,Ishiwatari A,ZHAO Zhong-yan,etal.Coesite-bearing granulite retrograded from eclogite inWeihai,eastern China[J].Eur J Mineral,1993,5:141-152.
[26]YOUNG Kyon Whoo.Petrological study of ultramaficrock in Choongnam Province,Korea[C]//Suh Man-cheol.Geological resources of the Yellow Sea.Kongju:Kongju National University,KOSEF,NSFC,1998:5-21.
[27]白景文,王文兴.黑龙江依兰牡丹江变质蓝片岩特征[J].岩石矿物学杂志,1988,7(4):298-308.BAI Jing-wen,WANG Wen-xing.The characteristics ofYilan-Mudanjiang metamorphic blueschist in Hei-longjiang[J].Acta Petrologica et Mineralogica,1988,7(4):298-308.
[28]曹熹,党增欣,张兴洲,等.佳木斯复合地体[M].长春:吉林科学技术出版社,1992:1-120.CAO Xi,DANG Zeng-xin,ZHANG Xing-zhou,et al.Jiamusi complex terrane[M].Changchun:Jilin Sci-ence&Technology Press,1992:1-120.
[29]吴福元,孙德有.佳木斯地块片麻状花岗岩的锆石离子探针U-Pb年龄[J].岩石学报,2001,17(3):443-452.WUFu-yuan,SUN De-you.Zircon SHRIMP U-Pb agesof gneissic granites in Jiamusi massif[J].Acta Petro-logica Sinica,2001,17(3):443-452.
[30]李锦轶.牛宝贵.黑龙江省东部中太古代碎屑岩浆锆石的发现及地质意义[J].地球学报,1995,3:331-333.LI Jin-yi,NIU Bao-gui.Discovery of Middle Archeanresidual zircon from eastern Heilongjiang and its geolog-ical implications[J].Acta Geoscientia Sinica,1995,3:331-333.
[31]李锦轶.中国东北及邻区若干地质构造问题的新认识[J].地质论平,1998,44(4):339-347.LI Jin-yi.Some new ideas on tectonics of NE China andits neighboring areas[J].Geology Review,1998,44(4):339-347.
[32]吴福元,曹林.东北亚地区的若干重要基础地质问题[J].世界地质,1999,18(2):1-13.WUFu-yuan,CAO Lin.Some important problems of ge-ology in northeastern Asia[J].Global Geology,1999,18(2):1-13.
[1]梁道俊,宋材秀.大地构造学[M].平壤:金日成综合大学出版社,2007:171-250.LYANG To Jun,Song Jae Su.Geotectonic geology[M].Pyongyang:Kim Il Sung University Press,2007:171-250.
[2]白龙浚.朝鲜地质[M].平壤:科学出版社,1998:1-160.BAEK Lyong Jun.Geology of Korea[M].Pyongyang:Science Press,1998:1-160.
[3]李炳柱.1∶250 000 Seoul-Namchonjeom地质图幅说明书[M].大田:韩国地质资源研究院,1999:1-64.LEE Byung Joo.Explanatory note of the 1∶250 000 Seoul-Namchonjeom sheet[M].Taejon:Korea Institute of Ge-ology,Mining and Materials,1999:1-64.
[4]李春昱.对亚洲地质构造发展的新认识[M].北京:科学出版社,1981:1-21.LI Chun-yu.Newideas of the tectonic development of A-sia[M].Beijing:Science Press,1981:1-21.
[5]任纪舜,王作勋.从全球看中国大地构造—中国及其邻区大地构造图简要说明[M].北京:地质出版社,1997:9-18.REN Ji-shun,WANG Zuo-xun.Tectonic of China asviewed over the globe—brief explanatory notes on the tec-tonic map of China and adjacent regions[M].Beijing:Geological Publishing House,1997:9-18.
[6]刘光鼎.中国海区及邻域地球物理场特征[M].北京:科学出版社,1992:1-150.LIU Guang-ding.Geophysical field features of China seaand adjacent regions[M].Beijing:Science Press,1992:1-150.
[7]Yin A,Nie S.An indentation mode for the North andSouth China collision and the development of the Tanluand Honamfaul systems,eastern Asia[J].Tectonics,1993,12:801-813.
[8]HAO Tian-yao,LIU Yi-ke,DUAN Chang.Characteris-tics of geophysical field in East China and adjacent re-gions[J].Geoscience Journal,1998,2(3):108-116.
[9]Suh Mancheol.Seismic stratigraphy of Henksan Basin inthe South Yellow Sea[C]//Suh Mancheol.Geologicalresources of the YellowSea.Kongju:Kongju National U-niversity,KOSEF,NSFC.1998:95-121.
[10]郝天珧,Suh Mancheol,王谦身,等.根据重力数据研究黄海周边断裂带在海区的延伸[J].地球物理学报,2002,45(3):385-398.HAO Tian-yao,Suh Mancheol,WANG Qian-shen,etal.The study of extension of faults in Yellow Sea andadjacent region from gravity data[J].Chinese Journalof Geophysics,2002,45(3):385-398.
[11]蔡乾忠.黄海含油气盆地区域地质与大地构造环境[J].海洋地质动态,2002,18(11):8-12.CAI Qian-zhong.Regional geology and geotectonic envi-ronment of petroliferous basins in the Yellow Sea[J].Marine Geology Letters,2002,18(11):8-12.
[12]戴明刚.黄海地质与地球物理特征研究进展[J].地球物理学进展,2003,18(3):583-591.DAI Ming-gang.Research progress in geology and geo-physics characters of the Yellow Sea[J].Progress inGeophysics,2003,18(4):583-591.
[13]郝天珧,刘建华,Suh Mancheol,等.黄海及邻区深部结构特点与地质演化[J].地球物理学报,2003,46(6):803-808.HAO Tian-yao,LIU Jian-hua,Suh Mancheol,et al.Deep structure characteristics and geological evolution inYellow Sea and adjacent region[J].Chinese Journal ofGeophysics,2003,46(6):803-808.
[14]郝天珧,Suh Mancheol,刘建华,等.黄海深部结构与中朝—扬子块体结合带在海区位置的地球物理研究[J].地学前缘,2004,11(3):51-61.HAO Tian-yao,Suh Mancheol,LIU Jian-hua,et al.Deep structure and boundary belt position between Sino-Korean and Yangtze blocks in Yellow Sea[J].EarthScience Frontiers,2004,11(3):51-61.
[15]葛肖虹,马文璞.东北亚南区中、新生代大地构造轮廓[J].中国地质,2007,34(2):212,222.GE Xiao-hong,MA Wen-pu.Mesozoic--Cenozoic frame-work of the southern Northeast Asia[J].Geology inChina,2007,34(2):212,222.
[16]秦蕴珊,赵一阳,陈丽蓉,等.黄海地质[M].北京:海洋出版社,1989:1-100.QIN Yun-shan,ZHAO Yi-yang,CHEN Li-rong,et al.Geology of Yellow Sea[M].Beijing:China OceanPress,1989:1-100.
[17]张文佑.中国海区及邻域海陆大地构造[M].北京:科学出版社,1986:575.ZHANG Wen-you.Marine and continental tectonics inChina seas and adjacent regions[M].Beijing:SciencePress,1986:575.
[18]杨志坚.胶东地块构造演化及其东延去向问题[J].海洋地质与第四纪地质,1989,9(2):1-11.YANG Zhi-jian.On the tectonic evolution of Jiaodongmassif and its extension to east[J].Marine Geologyand Quaternary Geology,1989,9(2):1-11.
[19]万天丰.中朝与扬子板块的鉴别特征[J].地质论评,2001,47(1):57-63.WAN Tian-feng.Distinctive characteristics of Sino-Ko-rean and Yangtze plates[J].Geological Review,2001,47(1):57-63.
[20]王谦身,安玉林.南黄海西部及邻域重力场与深部构造[J].科学通报,1999,44(22):2248-2453.WANG Qian-shen,AN Yu-lin.Gravity field and deepstructure in the western part of South YellowSea and ad-jacent area[J].Chinese Science Bulletion,1999,44(22):2448-2453.
[21]郝天珧,刘伊克,段昶.根据重磁资料探讨中国东部及其邻域断裂体系[J].地球物理学报,1996,39(增刊):141-149.HAO Tian-yao,LIUYi-ke,DUAN Chang.Approachingfault system of the East China and adjacent area fromgravity and magnetic data[J].Chinese Journal of Geo-physics,1996,39(Suppl.):141-149.
[22]蔡峰.北黄海盆地基底地质特征[J].海洋地质动态,1996,12(169):1-3.CAI Feng.Geological feature of the basement in theNorth Yellow Sea Basin[J].Marine Geology Letters,1996,12(169):1-3.
[23]陶宝国.南黄海周缘地区的地质构造联系[J].海洋地质译丛,1999,85(4):1-14.TAO Bao-guo.Relationship of geological tectonics a-round South Yellow Sea[J].Translation Collection ofMarine Geological,1999,85(4):1-14.
[24]CONG Bo-lin,ZHAI Ming-guo,Dennis C A,et al.Petrogenesis of ultrahigh-pressure rocks and their coun-try rock at Shuanghe in Dabieshan,central China[J].Eur J Mineral,1995,7:119-138.
[25]WANG Qing-chen,Ishiwatari A,ZHAO Zhong-yan,etal.Coesite-bearing granulite retrograded from eclogite inWeihai,eastern China[J].Eur J Mineral,1993,5:141-152.
[26]YOUNG Kyon Whoo.Petrological study of ultramaficrock in Choongnam Province,Korea[C]//Suh Man-cheol.Geological resources of the Yellow Sea.Kongju:Kongju National University,KOSEF,NSFC,1998:5-21.
[27]白景文,王文兴.黑龙江依兰牡丹江变质蓝片岩特征[J].岩石矿物学杂志,1988,7(4):298-308.BAI Jing-wen,WANG Wen-xing.The characteristics ofYilan-Mudanjiang metamorphic blueschist in Hei-longjiang[J].Acta Petrologica et Mineralogica,1988,7(4):298-308.
[28]曹熹,党增欣,张兴洲,等.佳木斯复合地体[M].长春:吉林科学技术出版社,1992:1-120.CAO Xi,DANG Zeng-xin,ZHANG Xing-zhou,et al.Jiamusi complex terrane[M].Changchun:Jilin Sci-ence&Technology Press,1992:1-120.
[29]吴福元,孙德有.佳木斯地块片麻状花岗岩的锆石离子探针U-Pb年龄[J].岩石学报,2001,17(3):443-452.WUFu-yuan,SUN De-you.Zircon SHRIMP U-Pb agesof gneissic granites in Jiamusi massif[J].Acta Petro-logica Sinica,2001,17(3):443-452.
[30]李锦轶.牛宝贵.黑龙江省东部中太古代碎屑岩浆锆石的发现及地质意义[J].地球学报,1995,3:331-333.LI Jin-yi,NIU Bao-gui.Discovery of Middle Archeanresidual zircon from eastern Heilongjiang and its geolog-ical implications[J].Acta Geoscientia Sinica,1995,3:331-333.
[31]李锦轶.中国东北及邻区若干地质构造问题的新认识[J].地质论平,1998,44(4):339-347.LI Jin-yi.Some new ideas on tectonics of NE China andits neighboring areas[J].Geology Review,1998,44(4):339-347.
[32]吴福元,曹林.东北亚地区的若干重要基础地质问题[J].世界地质,1999,18(2):1-13.WUFu-yuan,CAO Lin.Some important problems of ge-ology in northeastern Asia[J].Global Geology,1999,18(2):1-13.
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