2022 Vol. 37, No. 2
Article Contents

LI Sen, LIANG Jie, GONG Jianming, LIAO Jing, CHEN Jianwen, ZHANG Yinguo, WANG Jianqiang, YANG Chuansheng, YUAN Yong, LEI Baohua. Research progress of the Meso-Cenozoic sedimentary evolution in eastern Pakistan sea[J]. Marine Geology Frontiers, 2022, 38(2): 1-13. doi: 10.16028/j.1009-2722.2021.016
Citation: LI Sen, LIANG Jie, GONG Jianming, LIAO Jing, CHEN Jianwen, ZHANG Yinguo, WANG Jianqiang, YANG Chuansheng, YUAN Yong, LEI Baohua. Research progress of the Meso-Cenozoic sedimentary evolution in eastern Pakistan sea[J]. Marine Geology Frontiers, 2022, 38(2): 1-13. doi: 10.16028/j.1009-2722.2021.016

Research progress of the Meso-Cenozoic sedimentary evolution in eastern Pakistan sea

More Information
  • The East Pakistan sea area, located in the junction of three major plates of the world, has experienced complex tectonic-sedimentary evolution in history. Since Cenozoic era, the collision between the Indian plate and the Eurasian plate has been accelerated, that led to the rapid uplifting of the Himalaya, the form of the Indus deep-water fan, the second largest in the world, and the development of the sea off the Pakistan land. In addition to it, the area is heavily influenced by Indian monsoon as one of the two major monsoon regions in Asia. It is indeed the unique place in the world for study of the coupling relationship and interaction among the tectonic, sedimentary and climatic factors. Upon the basis of previous research results, we summarized in this paper the current research status of sedimentary evolution of the Mesozoic and Cenozoic basins in the Eastern Pakistan sea, put forward some main problems remained in controversy and made suggestions for future researches. Four main research interests and directions are put in front of us, i.e, the Indus fan since Miocene; the typical Meso-Cenozoic sedimentary geological bodies; the latest Quaternary turbidite sedimentology and the interaction of tectonic, sedimentation and climate. So far, few reports are available concerning the Mesozoic sediments beneath the Deccan basalt, the regional sedimentary evolution out of the depositional system, and the correlation of continental-marine sedimentary systems. Further investigations should be accelerated.

  • 加载中
  • [1] SCOTESE C R,GAHAGAN L M AND LARSON R L. Plate tectonic reconstructions of the Cretaceous and Cenozoic ocean basins[J]. Tectonophysics,1988,155(1/4):27-48. doi: 10.1016/0040-1951(88)90259-4

    CrossRef Google Scholar

    [2] CARMICHAEL S M,AKHTER S,BENNETT J K,et al. Geology and hydrocarbon potential of the offshore Indus Basin,Pakistan[J]. Petroleum Geoscience,2009,15(2):107-116. doi: 10.1144/1354-079309-826

    CrossRef Google Scholar

    [3] CHATTERJEE S,GOSWAMI A,SCOTESE C R. The longest voyage:tectonic,magmatic,and paleoclimatic evolution of the Indian plate during its northward flight from Gondwana to Asia[J]. Gondwana Research,2013,23(1):238-267. doi: 10.1016/j.gr.2012.07.001

    CrossRef Google Scholar

    [4] GAINA C,VAN HINSBERGEN D J J,SPAKMAN W. Tectonic interactions between India and Arabia since the Jurassic reconstructed from marine geophysics,ophiolite geology,and seismic tomography[J]. Tectonics,2015,34:875-906. doi: 10.1002/2014TC003780

    CrossRef Google Scholar

    [5] GAEDICKE C,PREXL A,SCHLÜTER H U,et al. Seismic stratigraphy and correlation of major regional unconformities in the northern Arabian Sea[J]. Geological Society,London,Special Publications,2002,195(1):25-36. doi: 10.1144/GSL.SP.2002.195.01.03

    CrossRef Google Scholar

    [6] SOLANGI S H,NAZEER A,ABBASI S A,et al. Morphological features of shelf margin:Examples from the Pakistan Offshore[J]. Geodesy and Geodynamics,2019,10:77-91. doi: 10.1016/j.geog.2018.09.004

    CrossRef Google Scholar

    [7] MCHARGUE T R,WEBB J E. Internal geometry,seismic facies,and petroleum potential of canyons and inner fan channels of the Indus submarine fan[J]. AAPG bulletin,1986,70(2):161-180.

    Google Scholar

    [8] CLIFT P,SHIMIZU N,LAYNE G,et al. Fifty-five million years of Tibetan evolution recorded in the Indus Fan[J]. Eos,Transactions American Geophysical Union,2000,81(25):277-281.

    Google Scholar

    [9] CLIFT P,CALVES G,GIOSAN L,et al. Climate and Tectonic Signals Preserved in the Indus Submarine Fan,Arabian Sea[J]. AGUFM,2007,2007:OS33A-0995.

    Google Scholar

    [10] KHIM B K,LEE J,HA S,et al. Variations in δ13C values of sedimentary organic matter since late Miocene time in the Indus Fan (IODP Site 1457) of the eastern Arabian Sea[J]. Geological Magazine,2020,157(6):1012-1021. doi: 10.1017/S0016756818000870

    CrossRef Google Scholar

    [11] GOMBOS A M,POWELL W G,NORTON I O. The tectonic evolution of western India and its impact on hydrocarbon occurrences:an overview[J]. Sedimentary Geology,1995,96:119-129. doi: 10.1016/0037-0738(94)00129-I

    CrossRef Google Scholar

    [12] MINSHULL T A,LANE C I,COLLIER J S,et al. The relationship between rifting and magmatism in the northeastern Arabian Sea[J]. Nature Geoscience,2008,1(7):463-467. doi: 10.1038/ngeo228

    CrossRef Google Scholar

    [13] KHAN M,LIU Y. Geodynamic evolution of the offshore Indus Basin Pakistan:the western Indian plate passive continental margin[J]. Geophysical Journal International,2019,217(2):1366-1386. doi: 10.1093/gji/ggz091

    CrossRef Google Scholar

    [14] KHAN M,ABDELMAKSOUD A. Unfolding impacts of freaky tectonics on sedimentary sequences along passive margins:Pioneer findings from western Indian continental margin (Offshore Indus Basin)[J]. Marine and Petroleum Geology,2020:104499.

    Google Scholar

    [15] KOLLA V,COUMES F. Morphology,internal structure,seismic stratigraphy,and sedimentation of Indus Fan[J]. AAPG Bulletin,1987,71(6):650-677.

    Google Scholar

    [16] KOLLA V, SCHWAB A M. Indus Fan: multi-channel seismic reflection images of channel-levee-overbank complexes[M]//Atlas of Deep Water Environments. Springer, Dordrecht, 1995: 100-104.

    Google Scholar

    [17] CLIFT P D,SHIMIZU N,LAYNE G D,et al. Development of the Indus Fan and its significance for the erosional history of the Western Himalaya and Karakoram[J]. Geological Society of America Bulletin,2001,113(8):1039-1051. doi: 10.1130/0016-7606(2001)113<1039:DOTIFA>2.0.CO;2

    CrossRef Google Scholar

    [18] GAEDICKE C,SCHLÜTER H U,ROESER H A,et al. Origin of the northern Indus Fan and Murray Ridge,Northern Arabian Sea:interpretation from seismic and magnetic imaging[J]. Tectonophysics,2002,355(1/4):127-143. doi: 10.1016/S0040-1951(02)00137-3

    CrossRef Google Scholar

    [19] CLIFT P,GAEDICKE C. Accelerated mass flux to the Arabian Sea during the middle to late Miocene[J]. Geology,2002,30(3):207-210. doi: 10.1130/0091-7613(2002)030<0207:AMFTTA>2.0.CO;2

    CrossRef Google Scholar

    [20] CLIFT P,GAEDICKE C,EDWARDS R,et al. The stratigraphic evolution of the Indus Fan and the history of sedimentation in the Arabian Sea[J]. Marine Geophysical Researches,2002,23(3):223-245. doi: 10.1023/A:1023627123093

    CrossRef Google Scholar

    [21] INAM A, TAHIR M. Channel-levee system-the major controlling mechanism for the sediment deposition on the Indus Fan[C]//Joint International Conference and First Annual Meeting of IGCP-475 DeltaMAP and APN project on the Mega-Deltas of Asia. 2004: 15-20.

    Google Scholar

    [22] KHAN N,REHMAN K,AHMAD S,et al. Sequence stratigraphic analysis of Eocene Rock Strata,Offshore Indus,southwest Pakistan[J]. Marine Geophysical Research,2016,37(3):207-228. doi: 10.1007/s11001-016-9280-5

    CrossRef Google Scholar

    [23] SHAHZAD K,BETZLER C,AHMED N,et al. Growth and demise of a Paleogene isolated carbonate platform of the Offshore Indus Basin,Pakistan:effects of regional and local controlling factors[J]. International Journal of Earth Sciences,2018,107(2):481-504. doi: 10.1007/s00531-017-1504-7

    CrossRef Google Scholar

    [24] SHAHZAD K,BETZLER C,QAYYUM F. Controls on the Paleogene carbonate platform growth under greenhouse climate conditions (Offshore Indus Basin)[J]. Marine and Petroleum Geology,2019,101:519-539. doi: 10.1016/j.marpetgeo.2018.12.025

    CrossRef Google Scholar

    [25] CLIFT P D. Controls on the erosion of Cenozoic Asia and the flux of clastic sediment to the ocean[J]. Earth and Planetary Science Letters,2006,241(3/4):571-580. doi: 10.1016/j.jpgl.2005.11.028

    CrossRef Google Scholar

    [26] PANDEY D K,CLIFT P D,KULHANEK D K,et al. Expedition 355 summary[J]. Proceedings of the International Ocean Discovery Program,2016:355.

    Google Scholar

    [27] 刘瑞璇,鹿化煜,王珧,等. 东阿拉伯海拉克希米盆地浊流沉积序列的粒度变化及其对中更新世气候转型的响应[J]. 第四纪研究,2018,38(5):1120-1129. doi: 10.11928/j.issn.1001-7410.2018.05.07

    CrossRef Google Scholar

    [28] 龚建明,廖晶,梁杰,等. 巴基斯坦海域油气勘探方向探讨[J]. 海洋地质前沿,2019,35(11):1-6.

    Google Scholar

    [29] 江凯禧,姚长华,郭清正,等. 印度扇深水区古—始新统烃源岩特征及发育模式[J]. 沉积学报,2016,34(4):785-793.

    Google Scholar

    [30] QAYYUM M,LAWRENCE R D,NIEM A R. Discovery of the palaeo-Indus delta-fan complex[J]. Journal of the Geological Society,1997,154(5):753-756. doi: 10.1144/gsjgs.154.5.0753

    CrossRef Google Scholar

    [31] GARZANTI E,CRITELLI S,INGERSOLL R V. Paleogeographic and paleotectonic evolution of the Himalayan Range as reflected by detrital modes of Tertiary sandstones and modern sands (Indus transect,India and Pakistan)[J]. Geological society of america bulletin,1996,108(6):631-642. doi: 10.1130/0016-7606(1996)108<0631:PAPEOT>2.3.CO;2

    CrossRef Google Scholar

    [32] BASTIA R, RADHAKRISHNA M. Sedimentation history and development of fan system along the continental margins of India[M]//Developments in Petroleum Science. Elsevier, 2012, 59: 127-160.

    Google Scholar

    [33] ELLOUZ-ZIMMERMANN N, LALLEMANT S J, CASTILLA R, et al. Offshore frontal part of the Makran Accretionary prism: The Chamak survey (Pakistan)[M]//Thrust belts and foreland basins. Springer, Berlin, Heidelberg, 2007: 351-366.

    Google Scholar

    [34] MÉTIVIER F,GAUDEMER Y,TAPPONNIER P,et al. Mass accumulation rates in Asia during the Cenozoic[J]. Geophysical Journal International,1999,137(2):280-318.

    Google Scholar

    [35] CALVÈS G. Tectono-stratigraphic and climatic record of the NE Arabian Sea[D]. Aberdeen: University of Aberdeen, 2009.

    Google Scholar

    [36] ZHUANG G,NAJMAN Y,GUILLOT S,et al. Constraints on the collision and the pre-collision tectonic configuration between India and Asia from detrital geochronology,thermochronology,and geochemistry studies in the lower Indus basin,Pakistan[J]. Earth and Planetary Science Letters,2015,432:363-373. doi: 10.1016/j.jpgl.2015.10.026

    CrossRef Google Scholar

    [37] CALVÈS G, SCHWAB A M, HUUSE M, et al. Seismic volcanostratigraphy of the western Indian rifted margin: the pre‐Deccan igneous province[J]. Journal of Geophysical Research: Solid Earth, 2011, 116(B1).

    Google Scholar

    [38] PRINS M A,POSTMA G,CLEVERINGA J,et al. Controls on terrigenous sediment supply to the Arabian Sea during the late Quaternary:the Indus Fan[J]. Marine Geology,2000,169(3/4):327-349. doi: 10.1016/S0025-3227(00)00086-4

    CrossRef Google Scholar

    [39] GOVIL P,NAIDU P D. Late Quaternary changes in depositional processes along the western margin of the Indus Fan[J]. Geo-Marine Letters,2008,28(1):1-6. doi: 10.1007/s00367-007-0083-1

    CrossRef Google Scholar

    [40] LIMMER D R,HENSTOCK T J,GIOSAN L,et al. Impacts of sediment supply and local tectonics on clinoform distribution:the seismic stratigraphy of the mid Pleistocene-Holocene Indus Shelf[J]. Marine Geophysical Research,2012,33(3):251-267. doi: 10.1007/s11001-012-9160-6

    CrossRef Google Scholar

    [41] BOURGET J,ZARAGOSI S,RODRIGUEZ M,et al. Late Quaternary megaturbidites of the Indus Fan:Origin and stratigraphic significance[J]. Marine Geology,2013,336:10-23. doi: 10.1016/j.margeo.2012.11.011

    CrossRef Google Scholar

    [42] CLIFT P D,GIOSAN L,HENSTOCK T J,et al. Sediment storage and reworking on the shelf and in the canyon of the Indus River‐fan system since the last glacial maximum[J]. Basin Research,2014,26(1):183-202. doi: 10.1111/bre.12041

    CrossRef Google Scholar

    [43] CLIFT P D,HODGES K V,HESLOP D,et al. Correlation of Himalayan exhumation rates and Asian monsoon intensity[J]. Nature geoscience,2008,1(12):875-880. doi: 10.1038/ngeo351

    CrossRef Google Scholar

    [44] NAJMAN Y. The detrital record of orogenesis:a review of approaches and techniques used in the Himalayan sedimentary basins[J]. Earth-Science Reviews,2006,74(1/2):1-72.

    Google Scholar

    [45] CURRAY J R. Sediment volume and mass beneath the Bay of Bengal[J]. Earth and Planetary Science Letters,1994,125(1/4):371-383. doi: 10.1016/0012-821X(94)90227-5

    CrossRef Google Scholar

    [46] KITOH A. Effects of mountain uplift on East Asian summer climate investigated by a coupled atmosphere-ocean GCM[J]. Journal of Climate,2004,17(4):783-802. doi: 10.1175/1520-0442(2004)017<0783:EOMUOE>2.0.CO;2

    CrossRef Google Scholar

    [47] ZHISHENG A,KUTZBACH J E,PRELL W L,et al. Evolution of Asian monsoons and phased uplift of the Himalaya-Tibetan plateau since Late Miocene times[J]. Nature,2001,411(6833):62-66. doi: 10.1038/35075035

    CrossRef Google Scholar

    [48] CLEMENS S,PRELL W,MURRAY D,et al. Forcing mechanisms of the Indian Ocean monsoon[J]. Nature,1991,353(6346):720-725. doi: 10.1038/353720a0

    CrossRef Google Scholar

    [49] RUDDIMAN W F. What is the timing of orbital-scale monsoon changes?[J]. Quaternary Science Reviews,2006,25(7/8):657-658. doi: 10.1016/j.quascirev.2006.02.004

    CrossRef Google Scholar

    [50] CLEMENS S C,Murray D W,Prell W L. Nonstationary phase of the Plio-Pleistocene Asian monsoon[J]. Science,1996,274(5289):943-948. doi: 10.1126/science.274.5289.943

    CrossRef Google Scholar

    [51] 孙国洪,田丽艳,李小虎,等. 西南印度洋中脊岩石地球化学特征及其岩浆作用研究[J]. 海洋地质与第四纪地质,2021,41(5):126-138.

    Google Scholar

    [52] 王小杰,颜中辉,刘俊,等. 基于模型优化的广义自由表面多次波压制技术在印度洋深水海域的应用[J]. 海洋地质与第四纪地质,2021,41(5):221-230.

    Google Scholar

    [53] 廖晶,龚建明,陈建文,等. 印度扇近海盆地重力滑动构造新发现[J]. 海洋地质前沿,2020,36(6):76-79.

    Google Scholar

    [54] 韩宗珠,孙苑高,王传,等. 西南印度洋中脊玄武岩地球化学特征及其对岩浆过程的指示意义[J]. 海洋地质前沿,2021,37(1):11-19.

    Google Scholar

  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Figures(10)

Article Metrics

Article views(2375) PDF downloads(219) Cited by(0)

Access History

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint