四川黑水-台湾花莲断面岩石圈与软流圈结构
|
摘要
运用现代构造解析理论和方法,对四川黑水—台湾花莲人工地震测深剖面与天然地震面波层析成像进行系统分析基础上,结合地质学、地球化学以及其它地球物理学标志等多学科综合研究显示,高速块体或幔块构造的几何结构样式是控制该区岩石圈构造格局和岩石圈表层构造变形最基本条件之一,首次建立起该断面岩石圈与软流圈结构模型,划分出岩石圈四种几何结构样式:克拉通陆根状结构,造山带楔状结构、碎块状结构和藕节状结构,以及岩石圈四类构造演化类型:克拉通型岩石圈、增厚型岩石圈、减薄型岩石圈和大洋型岩石圈。在系统论述断面及邻区岩石圈结构类型特征基础上,探讨了该断面软流圈结构特征、岩石圈与软流圈相互作用及其大陆动力学基本型式。
Using the theory and method of modern structural analysis, the paper analyses the artificial (seismic) sounding profiling and tomography of the natural seismic surface wave from Heishui of Sichuan to Hualian of Taiwan, and discovers that high-speed blocks varies in shape and differs in size in the lower lithosphere on the basis of the studies of the geological, geochemical, and geophysical signs. These blocks are termed mantle blocks. This shows that the tectonic pattern of the Heishui of Sichuan-Hualian of (Taiwan) lithosphere and the superficial deformation are basically controlled by the high-speed blocks or the mantle blocks. Based on the systematic studies of the high-speed blocks in the lithosphere, four geometric structural styles (craton-root-shaped, orogen-wedge-shaped, clastic-massive and slaty) are formulated for the first time, and four tectonic evolution types of the lithospheres (cratonic, thickening, thinning, and (oceanic)) are divided. According to the geometric models of the lithosphere from Heishui of Sichuan to Hualian Taiwan, the paper deduces the structural types of asthenosphere, the interaction of lithosphere and asthenosphere, and the continental dynamic types of lithosphere.
Using the theory and method of modern structural analysis, the paper analyses the artificial (seismic) sounding profiling and tomography of the natural seismic surface wave from Heishui of Sichuan to Hualian of Taiwan, and discovers that high-speed blocks varies in shape and differs in size in the lower lithosphere on the basis of the studies of the geological, geochemical, and geophysical signs. These blocks are termed mantle blocks. This shows that the tectonic pattern of the Heishui of Sichuan-Hualian of (Taiwan) lithosphere and the superficial deformation are basically controlled by the high-speed blocks or the mantle blocks. Based on the systematic studies of the high-speed blocks in the lithosphere, four geometric structural styles (craton-root-shaped, orogen-wedge-shaped, clastic-massive and slaty) are formulated for the first time, and four tectonic evolution types of the lithospheres (cratonic, thickening, thinning, and (oceanic)) are divided. According to the geometric models of the lithosphere from Heishui of Sichuan to Hualian Taiwan, the paper deduces the structural types of asthenosphere, the interaction of lithosphere and asthenosphere, and the continental dynamic types of lithosphere.
引文
[1]安德森DL.地球的理论[M].北京:地质出版社,1993.58-79.
[2]曹家敏,黄颐珍.爆炸地震研究华南地区邵阳-泉州地壳结构[A].阿尔泰-台湾地学断面论文集[C].武汉:中国地质大学出版社,1997.87-92.
[3]曹家敏,王有学.阿尔泰-台湾剖面茂汶-邵阳段地壳速度结构[A].阿尔泰-台湾地学断面论文集[C].武汉:中国地质大学出版社,1997.82-86.
[4]蔡学林,袁学诚.推覆构造与花岗岩成因问题[J].地质科技通报,1990,(5):32-36.
[5]蔡学林,邓明森,魏显贵.四川盆地褶皱构造接触应变分析[J].成都地质学院学报,1993,20(4):1-10.
[6]蔡学林,曹家敏,刘援朝,等.青藏高原多向碰撞-楔入隆升地球动力学模式[J].地学前缘,1999,6(3):181-189.
[7]蔡学林,朱介寿,曹家敏,等.东亚大陆巨型裂谷体系岩石圈与软流圈结构及动力学[J].中国地质,2002,29(3):234-245.
[8]陈培荣,华仁民,章邦桐,等.南岭燕山早期后造山花岗岩类:岩石学制约和地球动力学背景[J].中国科学D辑,2002,32(4):279-290.
[9]邓万明,黄萱,钟大赉.滇西新生代富碱斑岩的岩石特征与成因[J].地质科学,1998,33(4):412-425.
[10]张儒缓,从柏林.中国东南部新生代火山岩系及其超镁铁质岩包体[A].中国东部新生代玄武岩及深源岩石包体[C].北京:科学出版社,1987.349-439.
[11]郭令智.华南板块构造[M].北京:地质出版社,2001.192-215.
[12]胡圣标,汪屹华.黑水-泉州地学断面东段深部温度与岩石层厚度[J].地球物理学报,1994,37(3):331-337.
[13]何春荪.台湾地质概论台湾地质图说明书[M].台湾地质调查所出版,1986.
[14]金昕,周友松,曾建华.阿尔泰—台湾地学断面四川—湖南段岩石圈热结构分析与地质解释[A].阿尔泰—台湾地学断面论文集[C].武汉:中国地质大学出版社.1997.93-102.
[15]蒋洪堪,战双庆,王宏勋.四川大足—福建泉州深部地电特征[J].地球物理学报,1992,35(2):214-222.
[16]孔华,金振民,林源贤.道县玄武岩中麻粒岩包体的岩石学及年代学[J].长春科技大学学报,2000,30(2):115-119.
[17]刘光鼎.中国海域及邻域地质地球物理图集[M].北京:科学出版社,1993.56-91.
[18]刘援朝,钟应先.阿克塞—台湾断面显微构造研究[J].成都理工学院学报,1994,21(1):35-43.
[19]罗会文,杨光树.贵州镇远地区钾镁煌斑岩特征[J].岩石矿物学杂志,1989,(2):97-109.
[20]刘昌实,王汝成,舒良树,等.陆内S型花岗岩的形成与演化[A].中国东南部晚中生代花岗质火山—侵入杂岩成因与地壳演化[C].北京:科学出版社,2002.93-130.
[21]刘显凡,战新志,高振敏,等.云南六合深源包体与富碱斑岩成岩成矿的关系[J].中国科学D辑,1999,29(5):413-420.
[22]马杏垣.中国岩石圈动力学地图集[M].北京:中国地图出版社,1989.40-68.
[23]毛桐思,刘新美,赵明,等.地球内部层-圈耦合作用研究进展[J].科技导报,1999,(7):28-30.
[24]彭阜南,叶银灿,施斌,等.台湾海峡隧道地质与地震条件分析[J].高校地质学报,2001,7(2):175-188.
[25]任纪舜,王作勋,陈炳蔚,等.从全球看中国大地构造——中国及邻区大地构造图简要说明[M].北京:地质出版社,1998.1-38.
[26]石瑞诠,林正洪,赖宏亮,等.利用宽角震测资料模拟横跨台湾中部地壳构造之初步结果[J].地球科学集刊,1998,9(3):317-328.
[27]王方正,李红丽,朱勤文,等.湖南火山岩深源包体组合及岩石圈岩石学模型[J].地质科技情报,1997,16(3):1-7.
[28]汪屹华,卢华夏,贾东,等.闽西南里田推覆构造带的特征与围埔花岗岩的成因联系[A].东南大陆岩石圈结构与地质演化[C].北京:冶金工业出版社,1993.190-198.
[29]王懋基.黑水-泉州地学断面的重磁解释[J].地球物理学报,1994,37(3):321-329.
[30]许志琴,杨经绥,姜枚,等.大陆俯冲作用及青藏高原周缘造山带的崛起[J].地学前缘,1999,6(3):139-152.
[31]徐义刚.拉张环境中的大陆玄武岩浆作用:性质及动力学过程[A].化学地球动力学[C].北京:科学出版社,1999.119-167.
[32]徐夕生,周新民,O'ReillySY,等.中国东南部下地壳物质与花岗岩成因探索[J].岩石学报,1999,15(2):217-224.
[33]袁学诚,左愚,蔡学林,等.华南板块岩石圈构造与地球物理[A].八十年代中国地球物理学进展[C].北京:学术书刊出版社,1989.243-250.
[34]袁学诚,EgovovAS.北冰洋-欧亚大陆-太平洋地学断面及简要说明[M].北京:科学出版社,2000.1-32.
[35]叶义雄,石瑞诠,林正洪,等.台湾宽角海陆深部震测剖析[J].地球科学集刊,1998,9(3):301-316.
[36]于津海,徐夕生,周新民.华南沿海基性麻粒岩捕虏体的地球化学研究和下地壳组成[J].中国科学D辑,2002,32(5):383-393.
[37]朱介寿,曹家敏,李显贵,等.中国及其邻近地球三维结构初始模型的建立.地球物理学报,1997,40(5):627-648.
[38]朱介寿,曹家敏,蔡学林,等.东亚及西太平洋边缘海高分辨率面波层析成像[J].地球物理学报,2002,45(5):646-664.
[39]钟应先,刘援朝,蔡学林.湖南道县玄武岩中麻粒岩包体的初步研究[J].成都地质学院学报,1993,20(3):56-61.
[40]BousquetR,GofféB,HenryP,etal.Kinematic,thermalandpetrologicalmodeloftheCentralAlps:Lepontinemetamorphismintheuppercrustande-cologitisationofthelowercrust[J].Tectono-physics,1997,273:105-127.
[41]CaiXuelin,WeiXiangui,LiuYuanchao,etal.Onthewedging-inorogenesis[A].ProgressinGelogyofChina(1993-1996)-Papersto30thIGC[C].Bei-jing:ChinaOceanPress.314-320.
[42]ChemendaAI,YangRK,StephanJF,etal.Newresultsfromphysicalmodellingofarc-continentcol-lisioninTaiwan:evolutionarymodel[J].Tectono-physics,2001,333:159-178.
[43]HuangChiyue.StructuralevolutionfromPaleogeneextensiontolatestMiocene-Recentarc-continentCollisionoffshoreTaiwan:Comparisonwithonlandgeology[J].JournalofAsianEarthSciences,2001,19:619-639.
[44]DownesH.Shearzoneintheuppermantle-relationbetweengeochemicalenrichmentanddeformationinmantleperidotions[J].Geology,1990,18:374-377.
[45]LallemandS,FontY,BijwaardH,etal.Newin-sightson3-DPlatesinteractionnearTaiwanfromtomographyandtectonicimplications[J].Tectono-physics,2001,355:229-253.
[46]MenziesA.M.XuYigang.GeodynamicsoftheNorthChinaCraton[A].FlowerMFJ.MantleDynamicsandPlateInteractionsinEastAsia.Geo-phys[C].Washington:Geodynamicsser27,1998.155-165.
[47]PoupinetG,ThouvenotF,ZolotovEE,etal.TeleseismictomographyacrossthemiddleUrals:lithospherictraceofanancientcontinentalcollision[J].Tectonophysics,1997,276:19-33.
[48]SchmidSM,PfiffnerOA,FroitzheimN,etal.Geophysical-geologicaltransectandtectonicevolu-tionoftheSwiss-ItalianAlps[J].Tectonics,1996,15(5):1036-1064.
[49]TeixellA.CrustalstructureandorogenicmaterialbudgetinthewestCentralPyreness[J].Tectonics,1998,17(3):395-406.
[50]XuXisheng,O'ReillySY,GriffinWL,etal.TheNatureoftheCenozoicLithosphereatNushan,EastemChina[A].FlowrtMFJ.MantleDynamicsandPlateInteractionsinEastAsia[C].Washing-ton:GeodynamicsSer27,1998.167-195.
[2]曹家敏,黄颐珍.爆炸地震研究华南地区邵阳-泉州地壳结构[A].阿尔泰-台湾地学断面论文集[C].武汉:中国地质大学出版社,1997.87-92.
[3]曹家敏,王有学.阿尔泰-台湾剖面茂汶-邵阳段地壳速度结构[A].阿尔泰-台湾地学断面论文集[C].武汉:中国地质大学出版社,1997.82-86.
[4]蔡学林,袁学诚.推覆构造与花岗岩成因问题[J].地质科技通报,1990,(5):32-36.
[5]蔡学林,邓明森,魏显贵.四川盆地褶皱构造接触应变分析[J].成都地质学院学报,1993,20(4):1-10.
[6]蔡学林,曹家敏,刘援朝,等.青藏高原多向碰撞-楔入隆升地球动力学模式[J].地学前缘,1999,6(3):181-189.
[7]蔡学林,朱介寿,曹家敏,等.东亚大陆巨型裂谷体系岩石圈与软流圈结构及动力学[J].中国地质,2002,29(3):234-245.
[8]陈培荣,华仁民,章邦桐,等.南岭燕山早期后造山花岗岩类:岩石学制约和地球动力学背景[J].中国科学D辑,2002,32(4):279-290.
[9]邓万明,黄萱,钟大赉.滇西新生代富碱斑岩的岩石特征与成因[J].地质科学,1998,33(4):412-425.
[10]张儒缓,从柏林.中国东南部新生代火山岩系及其超镁铁质岩包体[A].中国东部新生代玄武岩及深源岩石包体[C].北京:科学出版社,1987.349-439.
[11]郭令智.华南板块构造[M].北京:地质出版社,2001.192-215.
[12]胡圣标,汪屹华.黑水-泉州地学断面东段深部温度与岩石层厚度[J].地球物理学报,1994,37(3):331-337.
[13]何春荪.台湾地质概论台湾地质图说明书[M].台湾地质调查所出版,1986.
[14]金昕,周友松,曾建华.阿尔泰—台湾地学断面四川—湖南段岩石圈热结构分析与地质解释[A].阿尔泰—台湾地学断面论文集[C].武汉:中国地质大学出版社.1997.93-102.
[15]蒋洪堪,战双庆,王宏勋.四川大足—福建泉州深部地电特征[J].地球物理学报,1992,35(2):214-222.
[16]孔华,金振民,林源贤.道县玄武岩中麻粒岩包体的岩石学及年代学[J].长春科技大学学报,2000,30(2):115-119.
[17]刘光鼎.中国海域及邻域地质地球物理图集[M].北京:科学出版社,1993.56-91.
[18]刘援朝,钟应先.阿克塞—台湾断面显微构造研究[J].成都理工学院学报,1994,21(1):35-43.
[19]罗会文,杨光树.贵州镇远地区钾镁煌斑岩特征[J].岩石矿物学杂志,1989,(2):97-109.
[20]刘昌实,王汝成,舒良树,等.陆内S型花岗岩的形成与演化[A].中国东南部晚中生代花岗质火山—侵入杂岩成因与地壳演化[C].北京:科学出版社,2002.93-130.
[21]刘显凡,战新志,高振敏,等.云南六合深源包体与富碱斑岩成岩成矿的关系[J].中国科学D辑,1999,29(5):413-420.
[22]马杏垣.中国岩石圈动力学地图集[M].北京:中国地图出版社,1989.40-68.
[23]毛桐思,刘新美,赵明,等.地球内部层-圈耦合作用研究进展[J].科技导报,1999,(7):28-30.
[24]彭阜南,叶银灿,施斌,等.台湾海峡隧道地质与地震条件分析[J].高校地质学报,2001,7(2):175-188.
[25]任纪舜,王作勋,陈炳蔚,等.从全球看中国大地构造——中国及邻区大地构造图简要说明[M].北京:地质出版社,1998.1-38.
[26]石瑞诠,林正洪,赖宏亮,等.利用宽角震测资料模拟横跨台湾中部地壳构造之初步结果[J].地球科学集刊,1998,9(3):317-328.
[27]王方正,李红丽,朱勤文,等.湖南火山岩深源包体组合及岩石圈岩石学模型[J].地质科技情报,1997,16(3):1-7.
[28]汪屹华,卢华夏,贾东,等.闽西南里田推覆构造带的特征与围埔花岗岩的成因联系[A].东南大陆岩石圈结构与地质演化[C].北京:冶金工业出版社,1993.190-198.
[29]王懋基.黑水-泉州地学断面的重磁解释[J].地球物理学报,1994,37(3):321-329.
[30]许志琴,杨经绥,姜枚,等.大陆俯冲作用及青藏高原周缘造山带的崛起[J].地学前缘,1999,6(3):139-152.
[31]徐义刚.拉张环境中的大陆玄武岩浆作用:性质及动力学过程[A].化学地球动力学[C].北京:科学出版社,1999.119-167.
[32]徐夕生,周新民,O'ReillySY,等.中国东南部下地壳物质与花岗岩成因探索[J].岩石学报,1999,15(2):217-224.
[33]袁学诚,左愚,蔡学林,等.华南板块岩石圈构造与地球物理[A].八十年代中国地球物理学进展[C].北京:学术书刊出版社,1989.243-250.
[34]袁学诚,EgovovAS.北冰洋-欧亚大陆-太平洋地学断面及简要说明[M].北京:科学出版社,2000.1-32.
[35]叶义雄,石瑞诠,林正洪,等.台湾宽角海陆深部震测剖析[J].地球科学集刊,1998,9(3):301-316.
[36]于津海,徐夕生,周新民.华南沿海基性麻粒岩捕虏体的地球化学研究和下地壳组成[J].中国科学D辑,2002,32(5):383-393.
[37]朱介寿,曹家敏,李显贵,等.中国及其邻近地球三维结构初始模型的建立.地球物理学报,1997,40(5):627-648.
[38]朱介寿,曹家敏,蔡学林,等.东亚及西太平洋边缘海高分辨率面波层析成像[J].地球物理学报,2002,45(5):646-664.
[39]钟应先,刘援朝,蔡学林.湖南道县玄武岩中麻粒岩包体的初步研究[J].成都地质学院学报,1993,20(3):56-61.
[40]BousquetR,GofféB,HenryP,etal.Kinematic,thermalandpetrologicalmodeloftheCentralAlps:Lepontinemetamorphismintheuppercrustande-cologitisationofthelowercrust[J].Tectono-physics,1997,273:105-127.
[41]CaiXuelin,WeiXiangui,LiuYuanchao,etal.Onthewedging-inorogenesis[A].ProgressinGelogyofChina(1993-1996)-Papersto30thIGC[C].Bei-jing:ChinaOceanPress.314-320.
[42]ChemendaAI,YangRK,StephanJF,etal.Newresultsfromphysicalmodellingofarc-continentcol-lisioninTaiwan:evolutionarymodel[J].Tectono-physics,2001,333:159-178.
[43]HuangChiyue.StructuralevolutionfromPaleogeneextensiontolatestMiocene-Recentarc-continentCollisionoffshoreTaiwan:Comparisonwithonlandgeology[J].JournalofAsianEarthSciences,2001,19:619-639.
[44]DownesH.Shearzoneintheuppermantle-relationbetweengeochemicalenrichmentanddeformationinmantleperidotions[J].Geology,1990,18:374-377.
[45]LallemandS,FontY,BijwaardH,etal.Newin-sightson3-DPlatesinteractionnearTaiwanfromtomographyandtectonicimplications[J].Tectono-physics,2001,355:229-253.
[46]MenziesA.M.XuYigang.GeodynamicsoftheNorthChinaCraton[A].FlowerMFJ.MantleDynamicsandPlateInteractionsinEastAsia.Geo-phys[C].Washington:Geodynamicsser27,1998.155-165.
[47]PoupinetG,ThouvenotF,ZolotovEE,etal.TeleseismictomographyacrossthemiddleUrals:lithospherictraceofanancientcontinentalcollision[J].Tectonophysics,1997,276:19-33.
[48]SchmidSM,PfiffnerOA,FroitzheimN,etal.Geophysical-geologicaltransectandtectonicevolu-tionoftheSwiss-ItalianAlps[J].Tectonics,1996,15(5):1036-1064.
[49]TeixellA.CrustalstructureandorogenicmaterialbudgetinthewestCentralPyreness[J].Tectonics,1998,17(3):395-406.
[50]XuXisheng,O'ReillySY,GriffinWL,etal.TheNatureoftheCenozoicLithosphereatNushan,EastemChina[A].FlowrtMFJ.MantleDynamicsandPlateInteractionsinEastAsia[C].Washing-ton:GeodynamicsSer27,1998.167-195.
版权所有：© 2023 中国地质图书馆 中国地质调查局地学文献中心