吉林大学学报(地球科学版) ›› 2016, Vol. 46 ›› Issue (2): 321-335.doi: 10.13278/j.cnki.jjuese.201602102

• 地质与资源 • 上一篇    下一篇

兰州盆地下白垩统碎屑岩层序地层序列:祁连山早白垩世隆升的沉积学响应

郭荣涛, 赵习, 刘红光, 石开波, 刘婧, 蒋启财   

  1. 北京大学地球与空间科学学院/石油与天然气研究中心, 北京 100871
  • 收稿日期:2015-08-09 发布日期:2016-03-26
  • 作者简介:郭荣涛(1983-),男,在站博士后,主要从事沉积学与地层学研究,E-mail:guorongtao0702@163.com
  • 基金资助:

    国家自然科学基金项目(41272137);中国地质调查局地质调查工作项目(1212011121268)

Sequence Stratigraphic Succession of the Lower Cretaceous Clastic Rock System in Lanzhou Basin: Sedimentological Response to the Early Cretaceous Uplift of Qilian Mountains

Guo Rongtao, Zhao Xi, Liu Hongguang, Shi Kaibo, Liu Jing, Jiang Qicai   

  1. School of Earth and Space Science/Oil & Gas Institute, Peking University, Beijing 100871, China
  • Received:2015-08-09 Published:2016-03-26
  • Supported by:

    Supported by National Natural Science Foundation of China(41272137)and Geological Survey Project of China Geological Survey(1212011121268)

摘要:

青藏高原东北缘的祁连山,在早白垩世期间发生明显隆升,受区域性构造运动和白垩纪特殊行星风系的影响,在山前盆地中沉积了一套特殊的碎屑岩序列。兰州盆地下白垩统发育完整,虽然局部被第四系覆盖,但总体出露良好,其特殊的相序单元构成的非常规体系域概念框架下的陆相层序地层学模式,对研究祁连山隆升的沉积学响应及环境效应具有重要意义。兰州盆地下白垩统为河口群,可以识别出5个三级层序(S.1-S.5),包括LAST和HAST两个非常规体系域,冲积扇和河流相粗碎屑沉积构成三级层序的LAST单元,HAST单元由湖泊相细碎屑地层组成。河口群上部地层发育的风成砂岩序列,在一定程度上可以解释为祁连山隆升造成的"焚风效应"产物,对研究祁连山的阶段性隆升特征具有重要的意义。早、晚白垩世之交,祁连山开始快速强烈隆升,兰州盆地整体抬升为剥蚀区,导致研究区缺失上白垩统。因此,兰州盆地下白垩统特殊的层序地层序列,不仅是早白垩世祁连山隆升的物质记录,还为研究早白垩世东亚大气环流格局变化提供了物质基础。

关键词: 祁连山隆升, 白垩系, 层序地层, 沉积学响应, 兰州盆地

Abstract:

Controlled by the uplift of Qilian Mountains and the change of climate, a set of clastic rocks are developed in Early Cretaceous in the continental basins in front of Qilian Mountains. The Cretaceous strata are developed and outcropped well in Lanzhou basin, which are made up of particular sedimentary facies successions under the framework of the unconventional system tracts, and are very important to the study of the Qilian Mountains uplift and their impacts on the Asian environment. The Lower Cretaceous Hekou Group can be divided into 5 third-order sequences (S.1-S.5), and every third-order sequence contains LAST and HAST unconventional systems. Alluvial fan facies and fluvial facies coarse clastic rocks constitute the LAST;while the HAST is composed by alluvial fan facies. The eolian sandstones in the Upper Part of Hekou Group are the products of "foehn effect" caused by the Qilian Mountains uplift. In the transition period of Early to Late Cretaceous, Qilian Mountains uplifted fast and intensively, which caused the denuded zone of the study area;so the Upper Cretaceous strata were not developed. The Lower Cretaceous sequences of Lanzhou basin are the material records of not only the Qilian Mountains uplift, but also the reconstruction of the pattern of the atmospheric circle in East Asia.

Key words: uplift of Qilian Mountains, Cretaceous, sequence stratigraphy, response of sedimentary, Lanzhou basin

中图分类号: 

  • P544.4

[1] 苏建平,吴保祥,雷怀彦,等.甘肃酒西白垩纪盆地沉积构成及盆地演化动力学分析[J].沉积学报,2002,20(4):568-573. Su Jianping, Wu Baoxiang, Lei Huaiyan, et al. The Sedimentary Formation and Analyses for Dynamic Evolution of Jiuxi Cretaceous Basin, Gansu Province[J]. Acta Sedimentologica Sinica, 2002, 20(4):568-573.

[2] 李奋其.中国西北部南北向伸展构造存在的新证据:酒泉早白垩世半地塑断陷成因初探[J].沉积与特提斯地质,2003,23(2):35-42. Li Fenqi. New Evidences for the Presence of the NS Trending Extensional Structures in Northwestern China:An Example from the Early Cretaceous Half Graben Fault Depressions in Jiuquan, Gansu[J]. Sedimentary Geology and Tethyan Geology, 2003, 23(2):35-42.

[3] 王晓丰,张志诚,郭召杰,等.酒西盆地南缘旱峡早白垩世火山岩地球化学特征及其构造意义[J].高校地质学报,2004,10(4):569-576. Wang Xiaofeng, Zhang Zhicheng, Guo Zhaojie, et al. Geochemical Characteristics and Tectonic Significance of the Early Cretaceous Volcanic Rocks in the Southern Margin of Jiuxi Basin[J]. Geological Journal of China Universities, 2004, 10(4):569-576.

[4] 王崇孝,马国福,周在华.酒泉盆地中、新生代构造演化及沉积充填特征[J].石油勘探与开发,2005,32(1):33-36. Wang Chongxiao, Ma Guofu, Zhou Zaihua. Structure Evolution and Sedimentary Filling of Jiuquan Basin in Mesozoic-Cenozoic Period, NW China[J]. Petroleum Exploration and Development, 2005, 32(1):33-36.

[5] 李明杰,谢结来,潘良云.祁连山北缘冲断带西段构造特征[J].地学前缘,2005,12(4):438-444. Li Mingjie, Xie Jielai, Pan Liangyun. Structural Character of Western Part of Northern Qilian Mountain Front Thrust Belt[J]. Earth Science Frontiers, 2005, 12(4):438-444.

[6] 刘宝睿,杨克绳,刘东艳.论河西走廊陆盆的演化和最终形成期[J].地质论评,2009,55(1):25-31. Liu Baorui, Yang Kesheng, Liu Dongyan. A Discussion on Evolution and Final Forming Time of the Hexi Corridor Continental Basin[J]. Geological Review, 2009, 55(1):25-31.

[7] 甘肃省地质矿产局.甘肃省区域地质志[M].北京:地质出版社,1989. Bureau of Geology and Mineral Resources of Gansu Province. Regional Geology of Gansu Province[M]. Beijing:Geological Publishing House, 1989.

[8] 杨雨.甘肃省岩石地层[M].武汉:中国地质大学出版社,1997. Yang Yu. Stratigraphy (Lithostratic) of Gansu Province[M]. Wuhan:China University of Geosciences Press, 1997.

[9] 张二朋,顾其昌,郑文林.西北区区域地层[M].武汉:中国地质大学出版社,1998. Zhang Erpeng, Gu Qichang, Zheng Wenlin. Regional Stratigraphy in Northwest China[M]. Wuhan:China University of Geosciences Press, 1998.

[10] 陈军,柳永清,旷红伟,等.甘肃兰州民和盆地中铺地区河口群沉积特征及其盆地分析意义[J].古地理学报,2013,15(2):155-168. Chen Jun, Liu Yongqing, Kuang Hongwei, et al. Sedimentary Characteristics and Their Basin Analysis Significance of the Lower Cretaceous Hekou Group in Zhongpu Area of Lanzhou-Minhe Basin, Gansu Province[J]. Journal of Paleogeography, 2013, 15(2):155-168.

[11] 牛绍武.甘肃酒泉盆地晚期中生代地层[J].地层学杂志,1987,11(1):1-22. Niu Shaowu. Late-Mesozoic Strata of Jiuquan Basin in Gansu Province[J]. Journal of Stratigraphy, 1987, 11(1):1-22.

[12] 姚金福,朱莲芳.酒西盆地西北地区晚侏罗早白垩世沉积相研究[J].沉积学报,1989,7(4):105-111. Yao Jinfu, Zhu Lianfang. A Sedimentary Facies Study of Late Jurassic to Early Cretaceous Epoch of Shibei District in Jiuxi Basin, Gansu[J]. Acta Sedimentologica Sinica, 1989, 7(4):105-111.

[13] 张琴,朱筱敏,张建军,等.酒西盆地青南凹陷柳沟庄一窟窿山地区下白垩统震积岩的发现及意义[J].地质学报,2003,77(2):158-162. Zhang Qin, Zhu Xiaomin, Zhang Jianjun, et al. The Discovery of Seismite and Its Significance in Lower Cretaceous in Liugouzhuang and Kulongshan Region, Qingnan Sag, Jiuxi Basin[J].Acta Geologica Sinica, 2003, 77(2):158-162.

[14] 王晓丰,张志诚,郭召杰,等.酒西盆地早白垩世沉积特征及原型盆地恢复[J].石油与天然气地质,2008,29(3):303-311. Wang Xiaofeng, Zhang Zhicheng, Guo Zhaojie, et al. Sedimentary Characteristics of the Lower Cretaceous and Reconstruction of the Prototype Basin in the Jiuxi Basin[J]. Oil & Gas Geology, 2008, 29(3):303-311.

[15] 彭楠,旷红伟,柳永清.北祁连-酒西地区早白垩世盆地沉积特征与古地理演化[J].地学前缘,2011,18(4):77-87. Peng Nan, Kuang Hongwei, Liu Yongqing. Sedimentary Evolution and Palaeogeography of the Early Cretaceous Basins from the Northern Qilian Mountains to Jiuxi Areas[J]. Earth Science Frontiers, 2011, 18(4):77-87.

[16] 薛沛霖,旷红伟,柳永清,等.甘肃酒泉西部地区下白垩统下沟组-中沟组沉积相特征与早白垩世盆地演化[J].地质通报,2013,32(2):476-487. Xue Peilin, Kuang Hongwei, Liu Yongqing, et al. Sedimentary Facies of the Early Cretaceous Xiagou Formation and Zhonggou Formation and Basin Evolution in Western Jiuquan, Gansu Province[J]. Geological Bulletin of China, 2013, 32(2/3):476-487.

[17] 冯益民,何世平.祁连山及其邻区大地构造基本特征:兼论早古生代海相火山岩的成因环境[J].西北地质科学,1995,16(1):92-103. Feng Yimin, He Shiping. Basic Characteristics of Tectonics in the Qilian Mountains and Its Neighbourins:On Genetic Environments of Early Paleozoic Marine Volcanics[J]. Northwest Geoscience, 1995, 16(1):92-103.

[18] 冯益民.祁连造山带研究概况:历史、现状及展望[J].地球科学进展,1997,12(4):307-314. Feng Yimin. Investigatory Summary of the Qilian Orogenic Belt, China:History, Presence and Prospect[J]. Advance in Earth Sciences, 1997, 12(4):307-314.

[19] 付国民,李永军,梁志录.酒西白垩纪盆地沉积构成及盆地演化动力学分析[J].沉积与特提斯地质,2003,23(1):31-36. Fu Guomin, Li Yongjun, Liang Zhilu. The Depositional Architectures and Geodynamics of the West Jiuquan Basin, Gansu[J]. Sedimentary Geology and Tethyan Geology, 2003, 23(1):31-36.

[20] 李海兵,杨经绥.青藏高原北部白垩纪隆升的证据[J].地学前缘,2004,11(4):345-359. Li Haibing, Yang Jingsui. Evidence for Cretaceous Uplift of the Northern Qinghai-Tibetan Plateau[J]. Earth Science Frontiers, 2004, 11(4):345-359.

[21] 李奋其,王成善,王崇孝.酒泉早白垩世盆地群构造特征和成因[J].地质学报,2006,80(2):181-191. Li Fenqi, Wang Chengshan, Wang Chongxiao. Tectonic Characteristics and Origin of Jiuquan Basin Group[J].Acta Geologica Sinica, 2006, 80(2):181-191.

[22] 李海兵,杨经绥,许志琴,等.阿尔金断裂带对青藏高原北部生长、隆升的制约[J].地学前缘,2006,13(4):59-79. Li Haibing, Yang Jingsui, Xu Zhiqin, et al. The Constraint of the Altyn Tagh Fault System to the Growth and Rise of the Northern Tibetan Plateau[J]. Earth Science Frontiers, 2006, 13(4):59-79.

[23] 唐玉虎,戴霜,黄永波,等.兰州民和盆地河口群沉积相和岩石磁化率:祁连山白垩纪隆升的记录[J].地学前缘,2008,15(2):261-271. Tang Yuhu, Dai Shuang, Huang Yongbo,et al.The Early Cretaceous Tectonic Uplift of Qilian Mountains:Evidence from the Sedimentary Facies and Susceptibility of Rocks of the Hekou Group, Lanzhou-Minhe Basin[J].Earth Science Frontiers,2008,15(2):261-271.

[24] Boyd R, Diessel C F K, Wadsworth J,et al.Development of a Nonmarine Sequence Stratigraphic Model[C]//American Association of Petroleum Geologist Annual Meeting. San Antonio:Official Program, 1999:A15.

[25] Bridge J S. Fluvial Facies Models:Recent Developments[C]//Posamentier H W, Walker R G. Facies Models Revisted. SEPM:Society for Sedimentary Geology, 2006:85-170.

[26] Catuneanu O. Principles of Sequence Stratigraphy[M]. Amsterdam:Elsevier, 2006:85-170.

[27] Catuneanu O, Abreu V, Bhattacharya J P, et al. Towards the Standardization of Sequence Stratigraphy[J]. Earth Science Reviews, 2009, 92:1-33.

[28] Ghazi S, Mountney N P.Facies and Architectural Element Analysis of a Meandering Fluvial Succession:The Permian Warchha Sandstone, Salt Range, Pakistan[J]. Sedimentary Geology, 2009, 221:99-126.

[29] 梅冥相.从正常海退与强迫型海退的辨别进行层序界面对比:层序地层学的进展之一[J].古地理学报,2010,12(5):549-564. Mei Mingxiang. Correlation of Sequence Boundaries According to Discerning Between Normal and Forced Regressions:The First Advance in Sequence Stratigraphy[J]. Journal of Paleogeography, 2010, 12(5):549-564.

[30] 吴因业,张天舒,张志杰,等.沉积体系域类型、特征及石油地质学意义[J].古地理学报,2010,12(1):69-81. Wu Yinye, Zhang Tianshu, Zhang Zhijie, et al. Types and Characteristics of Depositional Systems Tract and Its Petroleum Geological Significance[J]. Journal of Paleogeography, 2010, 12(1):69-81.

[31] Jinnah Z A, Roberts E M. Facies Associations, Paleoenvironment, and Base-Level Changes in the Upper Cretaceous Wahweap Formation, Utah, USA[J]. Journal of Sedimentary Research, 2011, 81:266-283.

[32] Hajek E A, Heller P L. Flow-Depth Scaling in Alluvial Architecture and Nonmarine Sequence Stratigraphy:Example from the Castlegate Sandstone, Central Utah, USA[J]. Journal of Sedimentary Research, 2012, 82:121-130.

[33] 葛肖虹,刘俊来.北祁连造山带的形成与背景[J].地学前缘,1999,6(4):223-230. Ge Xiaohong, Liu Junlai. Formation and Tectonic Background of the Northern Qilian Orogenic Belt[J]. Earth Science Frontiers, 1999, 6(4):223-230.

[34] 李麒麟,颉贵琴,周玲琦,等.兰州-民和盆地河口群层序地层格架特征及盆地演化[J].沉积与特提斯地质,2002,22(4):73-78. Li Qilin, Xie Guiqin, Zhou Lingqi, et al. Sequence Stratigraphy Framework of the Hekou Group and Evolution of the Lanzhou-Minhe Basin[J]. Sedimentary Geology and Tethyan Geology, 2002, 22(4):73-78.

[35] Blair T C, Mcpherson J G. Alluvial-Fans and Their Natural Distinction from Rivers Based on Morphology, Hydraulic Processes, Sedimentary Processes, and Facies Assemblages[J]. Journal of Sedimentary Research, 1994, 64:450-489.

[36] Leleu S, Hartley A, Williams B P J. Large-Scale Alluvial Architecture and Correlation in a Triassic Pebbly Braided River System, Lower Wolfville Formation (Fundy Basin, Nova Scotia, Canada)[J]. Journal of Sedimentary Research, 2009, 79:265-286.

[37] Davis D, Suppe J, Dahlen F A. Mechanics of Fold and Thrust Belts and Accretionary Wedges[J]. Journal of Geophysical Research, 1983, 88(B2):1153-1172.

[38] Beaumont C, Philippe F, Hamilton J. Erosional Control of Active Compressional Orogens[M]//McClay. Thrust Tectonics. London:Chapman & Hall, 1992:1-18.

[39] Meigs A J,Burbank D W. Growth of the South Pyrenean Orogenic Wedge[J]. Tectonics, 1997, 16:239-258.

[40] Boyer S E. Sendimentary Basin Taper as a Factor Controlling the Geometry and Advance of Thrust Belts[J]. American Journal of Science, 1995, 295:1220-1254.

[41] Mugnier J L, Baby P, Colletta B, et al. Thrust Geometry Controlled by Erosion and Sedimentation:A View from Analogue Models[J]. Geology, 1997, 25(5):427-430.

[42] Schlunegger F. Controls of Surface Erosion on the Evolution of the Alps:Constraints from the Stratigraphies of the Adjacent Foreland Basins[J]. International Journal of Earth Science, 1999, 88:285-304.

[43] Schlunegger F, Simpson G. Possible Erosional Control on Lateral Growth of the European Central Alps[J]. Geology, 2002, 30(10):907-910.

[44] 牛树银,孙爱群,白文吉.造山带与相邻盆地间物质横向迁移[J].地学前缘,1995,2(1):85-92. Niu Shuyin, Sun Aiqun, Bai Wenji. Lateral Migration of the Lithospheric Material Between Orogenic Zones and Adjacent Basins[J]. Earth Science Frontiers, 1995, 2(1):85-92.

[45] 李思田.沉积盆地的动力学分析:盆地研究领域的主要趋向[J].地学前缘,1995,2(3/4):1-8. Li Sitian. Geodynamics of Sedimentary Basins:The Main Trend of Basion Research[J]. Earth Science Frontiers, 1995, 2(3/4):1-8.

[46] 丁道桂,王道轩,刘伟新,等.西昆仑造山带与盆地[M].北京:地质出版社,1996. Ding Daogui, Wang Daoxuan, Liu Weixin, et al. The Western Kunlun Orogenic Belt and Basin[M]. Beijing:Geological Publishing House, 1996.

[47] 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. Liu Hefu, Xia Yiping, Yin Jinyin, et al. Coupling Mechanism of Strike-Slip Orogen and Basin[J]. Earth Science Frontiers, 1999, 6(3):121-132.

[48] 吴根耀,马力,钟大赉,等.滇桂交界区印支期增生弧型造山带:兼论与造山作用耦合的盆地演化[J].石油实验地质,2001,23(1):8-18. Wu Genyao, Ma Li, Zhong Dalai, et al. Indosinian Turkic-Type Orogen Bord Bordering Yunnan and Guangxi:With Reference to Coupled Basin Evolution[J]. Petroleum Geology & Experiment, 2001, 23(1):8-18.

[49] 吴根耀,马力.试论"盆""山"的耦合和脱耦及其运动学[J].石油实验地质,2003,25(2):99-109. Wu Genyao, Ma Li. An Approach to Orogenesis-Coupled/Decoupled Basin Development and Its Kinematics[J]. Petroleum Geology & Experiment, 2003, 25(2):99-109.

[50] 张原庆,钱祥麟.盆山耦合概念及机制[J].中国地质,2001,28(3):241-242. Zhang Yuanqing, Qian Xianglin. The Concept and Mechanism of Basin-Mountain Coupling[J]. China Geology, 2001, 28(3):241-242.

[51] 李继亮,肖文交,闫臻.盆山耦合与沉积作用[J].沉积学报,2003,21(1):52-60. Li Jiliang, Xiao Wenjiao, Yan Zhen. Basin-Range Coupling and Its Sedimentation[J]. Acta Sedimentologica Sinica, 2003, 21(1):52-60.

[52] Shanley K, McCabe P. Perspective on the Sequence Stratigraphy of Continental Strata[J]. American Association of Petroleum Geologists, Bulletin, 1994, 78:544-568.

[53] Plint A, McCarthy P, Faccini U. Nonmarine Sequence Stratigraphy:Updip Expression of Sequence Boundaries and Systems Tracts in a High-Resolution Framework, Cenomanian Dunvegan Formation, Alberta Foreland Basin, Canada[J]. American Association of Petroleum Geologists, Bulletin, 2001, 85:1967-2001.

[54] Holz M, Kalkreuth W, Banerjee I. Sequence Stratigraphy of Paralic Coal-Bearing Strata:An Overview[J]. International Journal of Coal Geology, 2002, 48:147-179.

[55] Arnott R W C, Zaitlin B A, Potocki D J. Stratigraphic Response to Sedimentation in a Net-Accommodation-Limited Setting, Lower Cretaceous Basal Quartz, South Central Alberta[J]. Bulletin of Canadian Petroleum Geology, 2002, 50(1):92-104.

[56] Olsen T, Steel R, Høgseth K, et al. Sequential Architecture in a Fluvial Succession:Sequence Stratigraphy in the Upper Cretaceous Mesaverde Group, Price Canyon, Utah[J]. Journal of Sedimentary Research, 1995, B65:265-280.

[57] Gibling M R, Tandon S K, Sinha R, et al. Discontinuity-Bounded Alluvial Sequences of the Southern Gangetic Plains, India:Aggradation and Degradation in Response to Monsoonal Strength[J]. Journal of Sedimentary Research, 2005, 75:369-385.

[58] Holbrook J M, Scott R W, Oboh-Ikuenobe F E. Base-Level Buffers and Buttresses:A Model for Upstream Versus Downstream Control on Fluvial Geometry and Architecture Within Sequences[J]. Journal of Sedimentary Research, 2006, 76:162-174.

[59] Mountney N P. Eolian Facies Models[M]//Posamentier H W, Walker R G. Facies Models Revisted. Tulsa:SEPM Special Publication, 2006:19-83.

[60] Nichols G. Aeolian Environments[M]//Nichols G. Sedimentology and Stratigraphy. Chichester of UK:Wiley-Blackwell, 2009:114-128.

[61] Marshall J R, Bull P A, Morgan R M. Energy Regimes for Aeolian Sand Grain Surface Textures[J]. Sedimentary Geology, 2012(253/254):17-24.

[62] Simpson E L, Hilbert-Wolf H L, Simpson W S, et al. The Interaction of Aeolian and Fluvial Processes During Deposition of the Upper Cretaceous Capping Sandstone Member, Wahweap Formation, Kaiparowits Basin, Utah, USA[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2008, 270:19-28.

[63] 梅冥相,苏德辰.青藏高原隆升的沉积学响应:来自甘肃酒泉地区新生代风成砂岩的启示[J].古地理学报,2013,15(3):351-361. Mei Mingxiang, Su Dechen. Sedimentological Response to Uplift of Qinghai-Tibet Plateau:A Contribution from Aeolian Sandstones of the Cenozoic in Jiuquan Area of Gansu Province[J]. Journal of Paleogeography,2013, 15(3):351-361.

[64] Skelton P W. The Cretaceous World[M]. London:Cambridge University Press, 2003.

[65] Sellwood B W, Valdes P J. Mesozoic Climates:General Circulation Models and the Rock Record[J]. Sedimentary Geology, 2006, 190:269-287.

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