盆山耦合与沉积盆地成因

王清晨; 李忠

盆山耦合与沉积盆地成因

王清晨,
李忠

中国科学院地质与地球物理研究所北京100029

基金项目: 国家重点基础研究发展规划 ( 973)项目 G19990 4330 3课题资助

详细信息

中图分类号: P512.2

计量

文章访问数: 677
HTML全文浏览量: 12
PDF下载量: 895
被引次数: 0

Basin-Orogen Coupling and Origin of Sedimentary Basins

Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029

摘要

摘要: 我国的沉积盆地成因研究主要遵循盆山耦合的研究思路进行 ,关注重点为盆山体系的构造、沉积和深部结构上的耦合现象。构造耦合研究是指盆山结合带的统一变形特征 ,沉积耦合研究是通过沉积响应去重塑盆山耦合过程及相邻造山带的演化过程 ,深部结构耦合的重点是研究盆山体系在岩石圈尺度的动力学统一性。国际上相应领域的研究重点为岩石圈深部过程与近地表构造过程的耦合。国内外研究既有相同之处 ,又有差异之处。建议在未来的沉积盆地成因研究中更加开阔思路 ,采用天然实验室的工作模式 ,进行多学科综合研究。
- 盆山耦合 /
- 盆地成因 /
- 国际岩石圈计划
Abstract: The study on origin of sedimentary basins in China followed approach of basin-orogen (range) coupling, including the structural and sedimentary coupling, as well as coupling in deep structure. The structural coupling can be revealed with deformation in the place at which basin and orogen (range) are jointed. The sedimentary coupling implies the tectonic-sedimentary responses that could reconstruct the orogenic process. The coupling in deep structure focuses on lithosphere dynamics revealed by deep structures. Parallel to this, international study on origin of sedimentary basins concentrated on coupling of lithosphere and near-surface processes. Keeping open eyes, integrating different approaches, and co-working in natural laboratories are all important in the future research on sedimentary basins.
- basin-orogen coupling /
- origin of sedimentary basins /
- International Lithosphere Program

HTML全文

参考文献(1)

[1]

［1］Bally A W, Snelson S. Realms of subsidence[A]. In: A D Miall ed. Facts and principles of world petroleum occurrence[C].Canadian Society of Petroleum Geologists Memoir 6, 1980.9～94.

［2］Klein G deV. Current aspects of basin analysis[J]. Sedimentary Geolog y, 1987, 50:95～118.

［3］Cloetingh S, Sassi W, Horvath F, et al. Basin analysis and dynam ics of sedimentary basin evolution[J]. Sediment Geol, 1993, 86:1～201.

［4］Zoback M D, Stephenson R A, Cloetingh S, et al. Stresses in the lithosphere and sedimentary basin formation[J]. Tectonophysics, 1993, 226:1～13

［5］Vilotte J P, Melosh J, Sassi W, et al. Lithosphere rheology and sedimentary basins[J]. Tectonophysics, 1993,226:89～95

［6］Quinlan G, Walsh J, Sassi W, et al. Relationship between deeper lithospheric processes and near-surface tectonics of basins[J]. Tectonophysic s, 1993, 226:217～225

［7］Nebauer F, Cloetingh S, Dinu C, et al. Tectonics of the Alpine- Carpathian-Pannonian region Ⅱ[J]. Tectonophysics, 1997, 272: 99～333

［8］Stephenson R A, Wilson M, De Boorder H, et al.EUROPROBE: Intrapl ate tectonics and basin dynamics of the Eastern European platform[J]. Tectonop hysics, 1996, 268:1～309

［9］Cloetingh S, Fernandez M, Munoz J A, et al. Structural controls on sedimentary basin evolution: introduction[J]. Tectonophysics, 1997,282: 10- 18

［10］Dickinson W, Anderson R N, Biddle K T, et al. The Dynamics of Sedimen tary Basins[J]. USGC, Washington D. C.: National Academy of Sciences, 1997.43 .

［11］Mascle A, Puigdefabregas C, Luterbacher H P, et al. Cenozoic Foreland Basins of Western Europe[C]. Geological Society, London, Special Publication London: Geological Society Publishing House. 1999

［12］叶连俊,孙枢. 沉积盆地的分类[J]. 石油学报,1980,1(3):1～6[Ye Lianjun a nd Sun Su. Classification of sedimentary basins[J]. Acta Petrolei Sinica, 1980 ,1(3):1～6]

［13］朱夏主编.中国中新生代盆地构造和演化[M]. 北京: 科学出版社. 1983, 230[Zhu X ia ed. Structure and Evolution of Mesozoic and Cenozoic Basins in China[M]. Be ijing: Science Press, 1983. 230]

［14］中国含油气区构造特征编委会. 中国含油气区构造特征[M]. 北京:石油工业出版社 ,1989. 320[Editorial Committee of Structural Features of Oil and Gas bearing a reas in China ed. Structural Features of Oil and Gas bearing areas in China[M] . Beijing: Petroleum Industry Press, 1989. 320]

［15］国家自然科学基金委员会地球科学部. 21世纪初地球科学战略重点[M]. 北京:中国科学技术出版社,2002.159[Department of Earth Sciences, NSFC, ed. Strategy of the Earth Science in the Beginning of the 21st Century[M]. Beijing: Chinese Sc ience and Technology Press, 2002. 159]

［16］李思田. 沉积盆地的动力学分析[J]. 地学前缘,1995,2(3-4): 1～8[Li Sitian. G eodynamics of Sedimentary Basins[J]. Earth Science Frontiers, 1995,2(3-4): 1～ 8]

［17］牛树银,孙爱群,白文吉. 造山带与相邻盆地间物质的横向迁移[J]. 地学前缘,199 5,2(1-2):85～92[Niu S, Sun A, Bai W. Lateral migration of the lithospheric material between orogenic zones and adjacent basins[J]. Earth Science Frontie rs, 1995,2(1-2):85～92]

［18］王玉新. 鄂尔多斯西缘褶皱-冲断带及其前陆盆地的形成与形变[D]. 北京:中国地质大学,1991[Wang Yuxin. Formation and Deformation of the Foreland Fold-Thrust belt in the Western Ordos[D]. Beijing: China University of Geosciences, 1991 ]

［19］刘和甫,梁慧社,蔡立国等. 天山两侧前陆冲断系构造样式与前陆盆地演化[J]. 地球科学,1994,19(6):727～741[Liu H, Liang H, Cai L, et al. Foreland thr ust system and basin evolution on both sides of the Tianshan Mountains[J]. Ear th Science Journal of China University of Geosciences, 1994, 19(6):727～741]

［20］刘和甫,梁慧杜,蔡立国等. 川西龙门山冲断系构造样式与前陆盆地演化[J]. 地质学报,1994,68(2):101～118[Liu H, Liang H, Cai L, et al. Foreland thru st system and basin evolution of the Longmenshan, Western Sichuan[J]. Acta Geo logica Sinica, 1994,68(2):101～118]

［21］Lu H, Jia D, Chen C, et al. Rejuvenation of the Kuqa foreland basin, nor thern flank of the Tarim Basin, Northern China[J]. International Geological Review, 1994, 36:1151～1158.

［22］卢华复,贾东,陈楚铭等. 库车新生代构造性质和变形时间[J]. 地学前缘,1999 ,6(4):215～221[Lu H, Jia D, Chen C, et al. Nature and timing of the Ku qa Cenozoic structures[J].Earth Science Frontiers, 1999, 6(4):215～221]

［23］李勇,曾允孚. 龙门山逆冲推覆作用的地层标识[J]. 成都理工学院学报,1995,22 (2):1～10[Li Y, Zeng Y. Stratigraphic signatures to thrusting of the Longmen M ountains thrust belt[J]. Journal of Chengdu Institute of Technology. 1995, 22 (2 ): 1～10]

［24］王清晨,从柏林,马力. 大别山造山带与合肥盆地的构造耦合[J]. 科学通报,1997, 42:575～580[Wang Q, Cong B, Ma L. Structural coupling of the Dabie Orogen with Hefei Basin[J]. Chinese Science Bulletin, 1997, 42, 575～580]

［25］张国伟,李三忠,刘俊霞等. 新疆伊犁盆地的构造特征与形成演化[J]. 地学前缘 ,1999,6(4):203～214[Zhang G, Li S, Liu J, et al. Structural feature and ev olution of Yili basin, Xinjiang[J]. Earth Science Frontiers, 1999, 6(4):203～21 4]

［26］李忠,李任伟,孙枢等. 合肥盆地南部侏罗系砂岩碎屑成分及其物源构造属性[J] .岩石学报,1999,15(3): 438～445[Li Z, Li R, Sun S, et al. Detrital co mposition and provenance tectonic attributes of Jurassic sandstone, south Hefei basin[J]. Acta Petrologica Sinica, 1999, 15(3): 438～445]

［27］郑洪波,Butcher K, Powell, C. 新疆叶城晚新生代山前盆地演化与青藏高原北缘的隆升[J]. 沉积学报,2002,20(2): 274～281[Zheng H, Butcher K, Powell C. Evolu tion of Neogene foreland basin in Yecheng, Xinjiang, and uplift of Northern Tibe tan Plateau[J]. Acta Sedimentologica Sinica, 2002,20(2): 274～281]

［28］刘和甫. 盆地-山岭耦合体系与地球动力学机制[J]. 地球科学,2001,26(6):581～5 96[Liu Hefu, Geodynamic scenario of coupled basin and mountain system[J]. Ear th Science, 2001, 26(6):581～596]

［29］汪泽成,刘和甫,熊宝贤等. 从前陆盆地充填地层分析盆山耦合关系[J]. 地球科学,2001,26(1):33～39[Wang Z, Liu H, Xiong B, et al. Basin-Mountain co upling analysis from filling stratigraphy of foreland basin [J]. Earth S cience Journal of China University of Geosciences, 2001, 26(1):33～39]

［30］刘和甫,夏义平,殷进垠等. 走滑造山带与盆地耦合机制[J]. 地学前缘,1999,6 (3 ):121～132[Li H, Xia Y, Yin J, et al. Coupling mechanism of strike- slip orogen and basin[J]. Earth Science Frontiers, 1999, 6(3 ):121～132.]

［31］刘和甫,汪泽成,熊保贤等. 中国中西部中、新生代前陆盆地与挤压造山带耦合分析 [J]. 地学前缘,2000,7(3): 55～72[Liu H, Wang Z, Xiong B, et al. Coupli ng analysis of Mesozoic-Cenozoic foreland basin and mountain system in Central and Western China[J]. Earth Science Frontiers, 2000, 7(3): 55～72]

［32］刘和甫,梁慧社,李晓清等. 中国东部中新生代裂陷盆地与伸展山岭耦合机制[J] . 地学前缘,2000,7(4): 477～486[Liu H, Liang H, Li X, et al. The couplin g mechanisms of Mesozoic-Cenozoic rift basins and extensional mountain system e astern China[J]. Earth Science Frontiers, 2000, 7(4): 477～486]

［33］Suppe J. Geometry and kinematics of fault bend folding[J]. Amer J Sci, 19 83, 283:684～721.

［34］Suppe J, Medwedeff D A. Geometry and kinematics of fault propagation foldi ng[J]. Ecologae Geol Helv, 1990, 83(3):409～454

［35］陆克政,漆家福,戴俊生等. 渤海湾新生代含油气盆地构造模式[M]. 北京:地质出版社,1997, 251[Lu K, Qi J, Dai J, et al. Tectonic model of Cenozoic p etroliferous basin Bohai Bay province[M]. Beijing: Geological Publishing Hou se, 251]

［36］马杏垣,刘和甫,王维襄. 中国东部中新生代裂陷作用和伸展构造[J]. 地质学报,1 983,57(1):22～32[Ma X, Liu H, Wang W. Mesozoic-Cenozoic rifting and extens ion in Eastern China[J]. Acta Geologica Sinica, 1983,57(1):22～32]

［37］王清晨,彭海波,孙枢. 赣北安源煤系沉积对构造活动的响应[J]. 地质科学,1991 ,1991,(3):231～238[Wang Q, Peng H, Sun S. Tectonic-sedimentation response of the Anyuan coal series, North Jiangxi[J]. Scientia Geologica Sinica, 1991,(3) :231～238]

［38］徐嘉炜. 论走滑断层作用的几个主要问题[J]. 地学前缘,1995,2(1-2): 125～136 [Xu J. Some major problems on strike-slip faulting[J]. Earth Science Frontie rs, 1995, 2(1-2): 125～136]

［39］朱光,王道轩,刘国生等. 郯庐断裂带的伸展活动及其动力学背景[J]. 地质科学 ,2001,36(3):269～278[Zhu G, Wang D, Liu G. Extensional activities along the Tan-Lu Fault Zone and its geodynamic setting[J]. Chinese Journal of Geology, 2001, 36(3):269～278]

［40］李忠,李任伟,孙枢. 大别山中生代构造演化:来自盆地充填记录的启示[J]. 地质通报,2002,21(8-9): 547～553[Li Z, Li R, Sun S. Mesozoic tectonic evoluti on of Dabie Mountains: Evidences from basin-fill records[J]. Geological Bull etin of China, 2002, 21(8-9): 547～553]

［41］李任伟,江茂生,李忠等. 大别山北麓侏罗系大理石砾石的碳-氧同位素组成及地质意义[J]. 岩石学报,1999,15(4): 623～629[Li R, Jiang M, Li Z, et al. Ca rbon and oxygen isotopic compositions of the marble conglomerates of Jurassic ag e in the northern margin of Dabie Mountains, China[J]. Acta Petrologica Sinica , 1999, 15(4): 623～629]

［42］郑永飞,傅斌,龚冰等. 大别山与榴辉岩共生大理岩的碳同位素异常[J]. 科学通报,1998,42: 2316～2320[Zheng Y, Fu B, Gong B, et al. Carbon isotope anom aly in marbles associated with eclogites from the Dabie Mountains in China[J] . Chinese Science Bulletin, 1998, 42: 2316～2320]

［43］王清晨,Rumble D.中国大别山双河超高压变质大理岩的氧、碳同位素[J].中国科学 (D辑),1999,29(3):214～221[Wang Q, Rumble D. Oxygen and carbon isotope co mposition from the UHP Shuanghe marbles, Dabie Mountains, China[J]. Science in China (Series D), 1999, 29(3):214～221]

［44］刘少峰,张国伟,张宗清等. 合肥盆地花岗岩砾石同位素年代学示踪[J]. 科学通报,2001,46(9): 477～486[Liu S, Zhang G, Zhang Z. Isotope chronological trac e of granite gravel in Hefei Basin[J]. Chinese Science Bulletin, 2001, 46(9): 477～486]

［45］王道轩,刘因,李双应等. 大别超高压变质岩折返至地表的时间下限:大别山北麓晚侏罗世砾岩中发现榴辉岩砾石[J]. 科学通报,2001,46(14): 1216～1220[Wang D, Liu Y, Li S. Lower time limit on the UHPM rock exhumation: Discovery of eclogite p ebbles in the Late Jurassic conglomerates from the northern foot of the Dabie Mo untains, eastern China[J]. Chinese Science Bulletin, 2001, 46(14): 1216～1220]

［46］Zhang P, Molnar P, Downs W R. Increased sedimentation rates and grain sizes 2±4 Myr ago due to the influence of climate change on erosion rates[J].Nature , 2002, 410: 891～897.

［47］Rea D K. Delivery of Himalayan sediment to the northern Indian Ocean and its relation to global climate, sea level, uplift, and seqwater strontium[J]. G eophys Monogr, 1992, 70: 387～402.

［48］李吉均,方小敏. 青藏高原隆起与环境变化研究[J]. 科学通报,1998, 13(15): 156 9～1574[Li J, Fang X. A research on uplift of the Tibetan plateau and environme nt change[J]. Chinese Science Bulletin, 1998, 13(15): 1569～1574]

［49］宋春晖,孙淑荣,方小敏等. 酒西盆地晚新生代沉积物重矿物分析与高原北部隆升[ J]. 沉积学报,2002,20(4): 552～559[Song C, Sun S, Fang X, et al. Analysis of tectonic uplift and heavy minerals of sediments on Jiuxi basin in the northe rn margin of Tibetan plateau since the Late Cenozoic[J]. Acta Sedimentologica Sinica, 2002, 20(4): 552～559]

［50］杨宝俊,张兴洲,孟令顺等. 中国大陆岩石圈结构篱笆图及其说明-1 0条GGT地球物理资料[J]. 长春科技大学学报,2001,31(4):385～390[Yang B, Zhang X, Meng L, et al. Fence diagram of lithosphere structure of China continent and its explanation -by using geophysical data of 10 GGTs[J]. Journal of Changchun U niversity of Science and Technology, 2001, 31(4):385～390]

［51］殷秀华,刘占坡,武翼新等. 青藏-蒙古高原东缘构造过渡带的布格重力场特征及地壳上地幔结构[J]. 地震地质,1988,10 (4):143～149[Yin X, Liu Z, Wu W, et a l. Bouguer field and structure of the crust-mantle around the Tibet -East Mo ngolia Plateau transition zone[J]. Seismology and Geology, 1988, 10 (4):143～1 49]

［52］高锐,黄东定,卢德源等. 横过西昆仑造山带与塔里木盆地结合带的深地震反射剖面 [J]. 科学通报,2000,45(17):1874～1879[Gao R, Huang D, Lu D, et al. D eep seismic reflection profile across the juncture zone between the Tarim Basin and the West Kunlun Mountains[J]. Chinese Science Bulletin, 2000, 45(17):1874 ～1879]

［53］高锐,肖序常,刘训等. 新疆地学断面深地震反射剖面揭示的西昆仑-塔里木结合带岩石圈细结构[J]. 地球学报,2001,22(6):547～552[Gao R, Xiao X, Liu X, et al. Detail lithospheric structure of the contact zone of west Kunlun and Tarim revealed by deep seismic reflection profile aong the Xinjiang geotransect[J] . Acta Geoscientia Sinica, 2001, 22(6), 547～552]

［54］贺日政,高锐,李秋生等. 新疆天山(独山子)-西昆仑(泉水沟)地学断面地震与重力联合反演地壳构造特征[J]. 地球学报,2001,22(6):553～558[He R, Gao R, Li Q, et al. Corridor gravity fields and crustal density structures in Tians han (Dushanzi) -West Kunlun (Quanshuigou) GGT[J]. Acta Geoscientia Sinica, 20 01, 22(6), 553～558]

［55］Ingersoll R V, Busby C J. Tectonic of sedimentary basins[A]. In: C J Busby and R V Ingersoll, eds. Tectonics of Sedimentary Basins[C]. Cambridge: Blackw ell Science, 1995,1～51.

［56］陈昌明,黄家宽,陈景山等. 第三纪渤海裂谷系的构造沉积演化特征[A]. 见:朱夏主编.中国中新生代盆地构造和演化[C].北京:科学出版社,1983,114～120[Chen C, H uang J, Chen J, et al. Tectono-sedimentation evolution of the Tertiary Boha i rift system[A]. In: Zhu Xia ed.Structure and Evolution of Mesozoic and Ce nozoic Basins in China[C]. Beijing: Science Press, 1983. 114～120]

［57］杨继良. 松辽断坳盆地的地质结构与油气[A]. 见:朱夏主编.中国中新生代盆地构造和演化[C].北京:科学出版社,1983.187～197[Yang J. Structure and oil-gas i n the Songliao Basin[A]. In: Zhu Xia ed. Structure and Evolution of Mesozoic and Cenozoic Basins in China[C]. Beijing: Science Press, 1983, 187～197

［58］Van der, Beek P A, Cloetingh S, Andriessen P A M. Mechanisms of extensional basin formation and vertical motions at rift flanks: constraints from tectonic modeling and fission track thermochronology[J]. Earth Planet Sci Lett, 1994, 1 21:417～433

［59］Zeyen H, Negredo A, Fernandez M. Extension with lateral material accommodati on[J]. Tectonophysics, 1996, 266:121～137.

［60］Roure F, Choukroune P, Polino R. Deep seismic reflection data and new insigh ts on the bulk geometry of mountain ranges C R Acad[J]. Sci Paris Ser iia, 199 6, 322:345～359

［61］Castle J W. Foreland-basin sequence response to collisional tectonism[J]. GSA Bulletin. 2001, 113:801～812.

［62］Angelier J. Tectonic analysis of fault slip data sets[J]. Journal of Geoph ysical Research, 1984, 89(B7), 5835～5848.

［63］Angelier J. Fault slip analysis and palaeostress reconstruction[A]. In: Ha ncock P L, ed. Continental Deformation[C]. Pergamon Press, Oxford, 1994, 53～1 00

［64］Cloetingh S, Burov E. Thermomechanical structure of European contimental li thosphere: constraints from rheological profiles and EET estimates[J]. Geophys J Int,1996,124:695～723.

［65］Bassi G. Relative importance of strain rate and rheology for the mode of con tinental extension[J]. Geophys J Int,1995, 122:195～210.

［66］Cloetingh S, d'Argenio B, Catalano R, et al. Interplay of extension and compression in basin formation[J]. Tectonophysics 1995, 252:1～484.

［67］Ter Voorde M, Cloetingh S. Numerical modeling of extension in faulted crust : effects of localized and regional deformation on basin stratigraphy[A]. In: Buchanan P G, Nieuwland D A, eds. Modern developments in structural interpretat ion, validation and modeling[C]. Geol Soc London Spec Publ, 1996, 99:283～296.

［68］Badescu D. Tectono-thermal regimes and lithosphere behaviour in the Externa l Dacides in the Upper Triassic and Jurassic Tethyan opening (Romanian Carpathia ns)[J]. Tectonophysics, 1997, 282: 167～188

［69］Cloetingh S, Ben Avraham Z, Sassi W, et al. Dynamics of extensional ba sins and inversion tectonics[J]. Tectonophysics, 1996, 266:1～523

[1]	王昕尧, 金振奎, 朱毅秀, 胡宗全, 刘光祥, 赵国伟, 李硕, 史书婷. 四川盆地自流井组陆相页岩石英成因研究 . 沉积学报, 2022, 40(4): 1010-1018. doi: 10.14027/j.issn.1000-0550.2021.053
[2]	李相博, 刘化清, 邓秀芹, 王雅婷, 龙礼文, 魏立花, 郝斌. 干旱环境河流扇概念与鄂尔多斯盆地延长组“满盆砂”成因新解 . 沉积学报, 2021, 39(5): 1208-1221. doi: 10.14027/j.issn.1000-0550.2020.077
[3]	尤东华, 韩俊, 胡文瑄, 陈强路, 曹自成, 席斌斌, 鲁子野. 塔里木盆地顺南501井鹰山组白云岩储层特征与成因 . 沉积学报, 2018, 36(6): 1206-1217. doi: 10.14027/j.issn.1000-0550.2018.092
[4]	高崇龙, 纪友亮, 高志勇, 王剑, 任影, 刘大卫, 段小兵, 桓芝俊, 程同冉. 准噶尔盆地腹部深层储层物性保存过程多因素耦合分析 . 沉积学报, 2017, 35(3): 577-591. doi: 10.14027/j.cnki.cjxb.2017.03.015
[5]	. 库车前陆盆地三叠系—新近系重矿物组合特征与盆山构造演化关系 . 沉积学报, 2014, 32(1): 68-77.
[6]	. 青藏高原北部新生代构造演化在柴达木盆地中的沉积记录 . 沉积学报, 2013, 31(05): 824-833.
[7]	. 西宁和贵德盆地新生代沉积物重矿物变化对构造活动的响应 . 沉积学报, 2013, 31(1): 139-148.
[8]	颜照坤. 龙门山前陆盆地晚三叠世沉积通量与造山带的隆升和剥蚀 . 沉积学报, 2010, 28(1): 91-101.
[9]	王家豪. 库车前陆盆地早白垩世岩石圈粘弹性变形的地层记录 . 沉积学报, 2010, 28(3): 412-418.
[10]	刘伟. 塔里木盆地台盆区中西部中下奥陶统鹰山组沉积环境研究 . 沉积学报, 2009, 27(3): 435-442.
[11]	陈守建. 昆仑造山带早—中泥盆世沉积特征及盆地性质探讨 . 沉积学报, 2008, 26(4): 541-551.
[12]	李玮. 新疆博格达山北缘晚古生代—中生代古水流样式转折及其构造意义 . 沉积学报, 2007, 25(2): 283-292.
[13]	李勇. 青藏高原东缘龙门山晚新生代走滑挤压作用的沉积响应 . 沉积学报, 2006, 24(2): 153-164.
[14]	戴传瑞, 张廷山, 郑华平, 叶舟, 梁兴, 姜照勇, 黄世伟, 胡清雄. 盆山耦合关系的讨论——以洞庭盆地与周边造山带为例 . 沉积学报, 2006, (5): 657-665.
[15]	. 盆山耦合关系的讨论——以洞庭盆地与周边造山带为例 . 沉积学报, 2006, 24(05): 657-665.
[16]	李继亮, 肖文交, 闫臻. 盆山耦合与沉积作用 . 沉积学报, 2003, 21(1): 52-60.
[17]	侯中健, 陈洪德, 田景春, 覃建雄, 彭军. 右江盆地海相泥盆系-中三叠统层序界面成因类型与盆地演化 . 沉积学报, 2000, 18(2): 205-209.
[18]	高振中, 何幼斌. 国际地质对比计划432项目(等深流沉积、底流与古环流研究)起动 . 沉积学报, 1998, 16(2): 154-154.
[19]	陶明信. 吐－哈盆地大地构造环境分析──兼论大陆板内盆地与造山带的成因关系 . 沉积学报, 1994, 12(4): 40-50.
[20]	黄杏珍. 介绍国际地质对比计划350项目（IGCP350）简况 . 沉积学报, 1994, 12(4): 140-140.

施引文献

资源附件(0)

访问统计

点击查看大图

计量

文章访问数: 677
HTML全文浏览量: 12
PDF下载量: 895
被引次数: 0

姓名
邮箱
手机号码
标题
留言内容
验证码

留言板

盆山耦合与沉积盆地成因

计量

Basin-Orogen Coupling and Origin of Sedimentary Basins

计量

目录

盆山耦合与沉积盆地成因

中国科学院地质与地球物理研究所北京100029

English Abstract

Basin-Orogen Coupling and Origin of Sedimentary Basins

Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

盆山耦合与沉积盆地成因

计量

出版历程

Basin-Orogen Coupling and Origin of Sedimentary Basins

计量

出版历程

目录

盆山耦合与沉积盆地成因

中国科学院地质与地球物理研究所 北京100029

English Abstract

Basin-Orogen Coupling and Origin of Sedimentary Basins

Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029

全文HTML

目录

友情链接

期刊在线

联系我们

中国科学院地质与地球物理研究所北京100029