晚侏罗世承德盆地砾岩碎屑源区分析及构造意义

和政军 牛宝贵 张新元. 晚侏罗世承德盆地砾岩碎屑源区分析及构造意义[J]. 岩石学报, 2007, 23(3): 655-666.
引用本文: 和政军 牛宝贵 张新元. 晚侏罗世承德盆地砾岩碎屑源区分析及构造意义[J]. 岩石学报, 2007, 23(3): 655-666.
Provenance analysis of the conglomerate clastic compositions from the Late Jurassic Chengde basin and its tectonic significance[J]. Acta Petrologica Sinica, 2007, 23(3): 655-666.
Citation: Provenance analysis of the conglomerate clastic compositions from the Late Jurassic Chengde basin and its tectonic significance[J]. Acta Petrologica Sinica, 2007, 23(3): 655-666.

晚侏罗世承德盆地砾岩碎屑源区分析及构造意义

  • 基金项目:

    国家自然科学重点基金项目(40132020)和中国地质调查局项目(1212010511502)资助成果.

Provenance analysis of the conglomerate clastic compositions from the Late Jurassic Chengde basin and its tectonic significance

  • 河北承德及寿王坟盆地在晚侏罗世土城子期堆积了大量的粗碎屑沉积.砾石成分统计结果显示,承德-寿王坟盆地充填的土城子组碎屑母岩组合主要有三种,其中火山岩、花岗质岩石和变质岩组合在承德盆地占绝对优势,反映了当时盆地以北的“内蒙地轴”为主要的蚀源区.向北逆冲的双庙断裂将承德盆地分成南北两个部分,断裂两侧的砾石成分组合基本相同,显示出碎屑物质共同来源于北部,同时也暗示了该断裂在土城子期可能没有强烈的活动(强烈活动期可能在土城子组之后?).分析表明,承德盆地南部的不对称向斜构造两侧砾石成分截然不同,说明该向斜构造控制了碎屑分布,是同沉积期形成的.该盆地南侧的碎屑供应量远远小于北侧,反映了控制盆地南缘发育的向北逆冲的灰窑断层可能是一条次要的同沉积断裂.在晚侏罗世整体向南推进的逆冲断裂系统中,灰窑断裂和双庙断裂应属于背向逆冲断层.承德盆地中大量的粗碎屑堆积与同期冲断带的耦合关系分析,指示了这一时期盆地北侧存在强烈的逆冲断裂活动.作为主要物源区,北部的“内蒙地轴”在晚侏罗世发生了强烈的隆升-剥蚀作用,推测当时在地貌上可能存在近E-W走向的古山系(或古高原?).
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  • [1]

    Bailey CM,Giorgis S and Coiner L.2002. Tectonic inversion and basement buttressing:An example from the Central Appalachian Blue Ridge province.Journal of Structural Geology,24:925-936

    [2]

    Brozovic N and Burbank DW.2000. Dynamic fluvial systems and gravel progradation in the Himalayan foreland.GSA Bulletin,112:394-412

    [3]

    Burbank DW and Raynolds RGH.1988. Stratigraphic keys to the Timing of Thrusting in Terrestrial Foreland Basins:Applications to the Northwestern Himalaya.In:Kleinsphn KL and Paola C (eds).New Perspectives in Basin Analysis.Springer-Verlag,New York Inc.,331 -351

    [4]

    Bureau of Geology and Mineral Resources of Hebei Province.1989. Regional Geology and Geological Maps (Scale 1:500,000) of Hebei Province,Beijing Municipality and Tianjin Municipality:Geological Memoirs,s.1,n.15. Beijing:Geological Publishing House,1 -741 (in Chinese with English abstract)

    [5]

    Cope Tand David GA.2003. Sedimentary evolution of the Yanshan foldthrust belt,northeast China.Ph.D.Thesis,Stanford University,Abstracts

    [6]

    Cope T.2004. Syntectonic sedimentary development of the Yanshan foldthrust belt,NE China:New constraints on thrust timing and geometry.32nd International Geological Congress,Florence:Scientific Sessions (part 1),abstracts,686

    [7]

    Cui SQ,Li JR,Wu ZH,Yi MC,Shen SM,Yin HR and Ma YS.2002. Mesozoic and Cenozoic Intracontinental Orogenesis of the Yanshan Area,China.Beijing:Geological Publishing House,1 -386 (in Chinese with English abstract)

    [8]

    Davis GA,Wang C,Zheng Y,Zhang J,Zhang C and Gehrels EG.1998. The enigmatic Yanshan fold-and-thrust belt of northern China:New views on its intraplate contractional styles:Geology,26:43-46

    [9]

    Davis GA,Zheng YD,Wang C,Darby BJ,Zhang CH and Gehrels G.2001. Mesozoic tectonic evolution of the Yanshan fold and thrust belt,with emphasis on Hebei and Liaoning provinces,northern China.Geological Society of America,Memoir,194:171 -197

    [10]

    Davis GA.2005. The late Jurassic "Tuchengzi/Houcheng" formation of the Yanshan fold-thrust belt:An analysis.Earth Science Frontiers,12 (4):331 -345

    [11]

    DeCelles PG,Gehrels GE,Quade J,Ojha TP,Kapp PA and Upreti BN.1998. Neogene foreland basin deposits,erosional unroofing,and the kinematic history of the Himalayan fold-thrust belt,western Nepal.GSA Bulletin,110:2-21

    [12]

    DeCelles PG.1988. Lithologic provenance modeling applied to the late Cretaceous synorogenic Echo Canyon Conglomerate,Utah:A case of multiple source areas.Geology,16:1039-1043

    [13]

    DeCelles P,Gray MB,Ridgway KD,Cole RB,Srivastava P,Pequera N and Pivnik DA.1991. Kinematic history of a foreland basin uplift from Paleogene synorogenic conglomerate,Beartooth Range,Wyoming and Montana.GSA Bulletin,103:1458-1475

    [14]

    Dickinson WR.1970. Interpreting detrital modes of graywacke and arkose.Jour.Sed.Petro.,40:695-707

    [15]

    Dickinson WR.1979. Plate tectonic and sandstone compositions.AAPG,63:2164 -2182

    [16]

    Dickinson WR.1983. Provenance of north American Phanerozoic sandstones in relation to tectonic setting.GSA Bulletin,94:222-235

    [17]

    Flemings PB and Jordan TE.1989. A synthetic stratigraphic model of foreland basin development.Journal of Geophysical Research,94 (B4):3851 -3866

    [18]

    Garfunkel Z and Greiling R O.2002. The implications of foreland basins for the causative tectonic loads.EGU Stephan Mueller Special Publication,Series 1:3-16

    [19]

    Hao YC,Su DY and Li YG.1982. Stratigraphical division of non-marine Cretaceous and the Jura-Cretaceous boundary in china.Acta Geologica Sinica,56 (3):187-199 (in Chinese with English abstract)

    [20]

    He ZJ and Niu BG.2004. Re-inquiring of the "Chengde Thrust Plate":Evidences from the Mesoproterozoic Changchengnian Sedimentary facies in the Yanshan Region.Geological Review,50 (5):464 -470 (in Chinese with English abstract)

    [21]

    He ZJ,Li JY,Niu BG and Ren JS.1998. An intense nappe-uplift event of late Jurassic in the Yanshan-Yinshan area,northern China and its sedimentary response.Geological Review,44 (4):407-418 (in Chinese with English abstract)

    [22]

    He ZJ,Niu BG and Zhang XY.2007. Late Jurassic thrusting and depositional basin systems in the Chaoyang region,western Liaoning.Geological Review (in press)

    [23]

    He ZJ,Wang ZQ and Ren JS.1999. A preliminary research on sedimentary features and genetic mechanism of frontal basins of the Jurassic large-scale nappe in the northern region of North China.Scientia Geologica Sinica,34 (2):186-195 (in Chinese with English abstract)

    [24]

    He ZJ.1990. Review on the research of the relation between sandstone detritus and plate tectonic setting.Geological Science and Technology Information,19(4):7 -12 (in Chinese with English abstract)

    [25]

    Ingersoll RV,Bullard TF,Ford RL,Grimm JP,Pickle JD and Sares SW.1984. The effect of grain size on detrital modes:A test of the Gazzi Dickinson point-counting method.Journal of Sedimentary Petrology,54:103-116

    [26]

    Ji Q,Chen W,Wang WL,Jin XC,Zhang JP,Liu YQ,Zhang H,Yao PY,Ji SA,Yuan CX,Zhang Y and You HL.2004. Mesozoic Jehol Biota of Western Liaoning,China.Beijing:Geological Publishing House,1 -375 (in Chinese)

    [27]

    Jones MA,Heller PL,Roca E,Garce M and Cabrera L.2004. Time lag of syntectonic sedimentation across an alluvial basin:theory and example from the Ebro Basin,Spain.Basin Research,16:467-488

    [28]

    Jordan TE,Flemings PB,and Beer JA.1988. Dating Thrust-fault activity by use of foreland -basin strata.In:Kleinsphn K L and Paola C (eds).New Perspectives in Basin Analysis.Springer-Verlag New York Inc.,307-330

    [29]

    Bureau of Geology and Mineral Resources of Liaoning Province.1989. Regional Geology and Geological Maps (Scale 1:500,000) of Liaoning Province:Geological Memoirs,s.1,n.14. Beijing:Geological Publishing House,1 856 (in Chinese with English abstract)

    [30]

    Li Z,Liu SF,Zhang JF,Li Z and Wang QC.2004. Late Jurassic basinfill record and its implication for basin margin tectonism,Chengde,Yanshan Mountains,North China.Earth Science Frontiers,11 (3):245 -254 (in Chinese with English abstract)

    [31]

    Mandal N,Chattopadhyay A and Bose S.1997. Imbricate thrust spacing:experimental and theoretical analyses.In:Sengupta,S.(ed)Evolution of Geological Structures in Macro-to Micro-scales.London:Chapman and Hall,143-165

    [32]

    McClay KR and Buchanan PG.1992. Thrust faults in inverted extensional basins.In:McClay KR (ed).Thrust Tectonics.London:Chapman & Hall,93-104

    [33]

    Morton BK,Constenius KN and DeCelles PG.2004. Tectonic control on coarse-grained foreland-basin sequences:An example from the Cordilleran foreland basin.Utah Geology,32 (7):637-640

    [34]

    Nemcok M,Schamel S and Gayer R.2005. Thrustbelts:Strucural Architecture,Thermal Regimes and Petrolenm Systems.London:Cambridge University Press,3 -25; 121 -135; 192-220

    [35]

    Nichols GJ.1987. Syntectonic alluvial fan sedimentation,southern Pyrenees.Geological Magazine,124(2):121-133

    [36]

    Niu BG,He ZJ,Song B,Ren JS and Xiao LW.2004. SHRIMP Geochronology of volcanics of the Zhangjiakou and Yixian Formations,Northern Hebei Province,with a discussion on the age of the Xing\' anling Group of the Great Hinggan Mountains and volcanic strata of the southeastern coastal area of China.Scientia Geologica Sinica (English Edition),78(6):1214 -1228

    [37]

    Pettijohn F J.1975. Sedimentary Rocks (Third Edition).New York:Harper & Row,1-628

    [38]

    Remane J.2000. Explanatory note to the international stratigraphic chart.Journal of stratigraphy,24 (Sup.):321 340 (in English and Chinese)

    [39]

    Schlunegger F,Jordan TE and Klaper EM.1997. Controls of erosional denudation in the orogen on foreland basin evolution:The Oligocene central Swiss Molasse Basin as an example.Tectonics,16(5):823-840

    [40]

    Schlunegger F,Melzer J and Tucker GE.2001. Climate exposed sourcerock lithologies,crustal uplift and surface erosion:A theoretical analysis calibrated with data from the Alps/North Alpine Foreland Basin system.Int.J.Earth Sci.(Geol Rundsch),90:484 -499

    [41]

    Sun ZM,Xu K,Ma XH,Liang HD,Yang TS,Yang ZY,Li RH,Li Y and Zhao Y.2003. Magnetostratigraphy of the Jurassic-Cretaceous boundary near bird-bearing in western Liaoning.Acta Geologica Sinica,76(3):317 -324 (in Chinese with English abstract)

    [42]

    Wang WL,Zhang H,Zhang LJ,Zheng SL,Yang FL,Li ZT,Zhen YJ and Ding QH.2004. Standard Stratigraphic Section of Tuchengzi Stage and Yixian Stage:Their Stratigraphy,Palaontology and Tectonic-Volcanic Actions.Beijing:Geological Publishing House,1 -514 (in Chinese with English abstract)

    [43]

    Zhang CH,Wu GG,Xu DB,Wang GH and Sun WH.2004b.Mesozoic tectonic framework and evolution in the central segment of the intraplate Yanshan orogenic belt.Geological Bulletin of China,23 (9-10):864-873 (in Chinese with English abstract)

    [44]

    Zhang CH,Xu DB,Zhang WJ,Cope TD,Wang GH,Sun WH,Xiao WF,Zhang ZY and Zhang JL.2004a.Syntectonic sedimentation analysis applied to the reconstruction of the thrusting deformation process:An example from the Mesozoic thrust tectonics in eastern Yanshan Orogenic belt,south of Lingyuan City,western Liaoning Province.Earth Science Frontiers,11 (3):227-242 (in Chinese with English abstract)

    [45]

    Zhao Y.1990. The Mesozoic orogenies and tectonic evolution of the Yanshan area.Geological Review,36:1 -13 (in Chinese with English abstract)

    [46]

    Zhao Y,Zhang QH,Xu G,Yang ZY and Hu JM.2004. Jurassic major tectonic events of the Yanshanian intraplate deformation belt.Geological Bulletin of China,23 (9-10):854-863 (in Chinese with English abstract)

    [47]

    崔盛芹,李锦蓉,吴珍汉,易明初,沈淑敏,尹华仁,马寅生.2002.燕山地区中新生代陆内造山作用.北京:地质出版社,1-386

    [48]

    郝诒纯,苏德英,李友桂等.1982.中国非海相白垩系的划分及侏罗-白垩系的分界.地质学报,56(3):187-199

    [49]

    和政军,牛宝贵.2004."承德逆掩片"之商榷--来自燕山地区中元古代长城系的沉积地质证据.地质论评,50(5):464-470

    [50]

    和政军,李锦轶,牛宝贵,任纪舜.1998.燕山阴山地区晚侏罗世强烈推覆隆升事件及沉积响应.地质论评,44(4):407-418

    [51]

    和政军,牛宝贵,张新元.2007.辽西朝阳地区的晚侏罗世逆冲断裂-沉积盆地系统.地质论评,(待刊)

    [52]

    和政军,王宗起,任纪舜.1999.华北北部侏罗纪大型推覆构造带前缘盆地沉积特征和成因机制初探.地质科学,34(2):186-195

    [53]

    和政军.1990.砂岩碎屑组分与板块构造位置关系的研究现状.地质科技情报(中国地质大学),9(4):7-12

    [54]

    河北省地矿局.1989.河北省区域地质志.北京:地质出版社,192-21;393-423

    [55]

    李忠,刘少峰,张金芳,王清晨.2003.燕山典型盆地充填序列及迁移特征:对中生代构造转折的影响.中国科学(D),33(10):931-940

    [56]

    辽宁省地矿局.1989.辽宁省区域地质志.北京:地质出版社,227-251

    [57]

    季强,陈文,王五力,金小赤,张建平,柳永清,张宏,姚培毅,姬书安,袁崇喜,张彦,尤海鲁.2004.中国辽西中生代热河生物群,北京:地质出版社,96-157

    [58]

    刘少峰,张金芳,李忠,王清晨.2004.燕山承德地区晚侏罗世盆地充填记录及对盆缘构造作用的指示.地学前缘,11(3):245-254

    [59]

    孙知明,许坤,马醒华,梁鸿德,杨天水,杨振宇,李荣辉,李瑜,赵越.2002.辽西朝阳地区含鸟化石层附近侏罗-白垩纪磁性地层研究,地质学报,76(3):317-324

    [60]

    王五力,张宏,张力君,郑少林,杨芳林,李之彤,郑月娟,丁秋红.2004.土城子阶、义县阶标准地层剖面及其地层古生物、构造-火山作用.北京:地质出版社,1-514

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修回日期:  2006-08-17
刊出日期:  2007-03-31

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