RESEARCH PAPER

Sedimentary environment and petrological features of organic-rich fine sediments in shallow water overlapping deposits: A case study of Cambrian Yuertus Formation in northwestern Tarim Basin, NW China

  • Zhimin JIN ,
  • Xiucheng TAN ,
  • Hao TANG ,
  • Anjiang SHEN ,
  • Zhanfeng QIAO ,
  • Jianfeng ZHENG ,
  • Fei LI ,
  • Shixuan ZHANG ,
  • Lei CHEN ,
  • Chenggang ZHOU
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  • 1. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Southwest Petroleum University, Chengdu 610500, China
    2. Key Laboratory of Carbonate Reservoir, CNPC, Hangzhou 310023, China
    3. Korla Branch of Geophysical Research Institute, BGP Inc., Korla 841000, China

Received date: 2019-08-07

  Revised date: 2020-02-26

  Online published: 2020-06-19

Supported by

China National Science and Technology Major Project(2016ZX05004002-001);National Natural Science Foundation of China(41602147)

Abstract

Taking the Cambrian Yuertus Formation outcrop profiles in the Aksu-Keping-Wushi areas of northwestern Tarim Basin as examples, the depositional environments of organic rich fine sediment were analyzed by examining the outcrop profiles macroscopically and microscopically. The study reveals that: (1) The lower part of the Yuertus Formation consists of organic-rich fine sediment or thin rhythmic interbeds of organic-rich fine sediment and siliceous sediment, the formation transforms to terrigenous diamictic grain shoal and inverse grading carbonate rocks upward. (2) The thin limestone interbedded with dark shale rhythmically has inverse grading. (3) The thin-bedded siliceous rock has metasomatic residual granular texture, stromatolithic structure and cementation fabric in vugs. (4) There are iron crust layers at the top of the shallowing diamictic grain shoal, beneath which exposed karst signs, such as karrens, dissolved fissures, sack-like vugs, near surface karst (plastic) breccia, breccia inside the karst system and terrigenous clastic fillings, can be seen. (5) Both the outcrops and seismic profiles show that organic-rich fine sediments above the unconformities or exposed surfaces are characterized by overlapping. The organic-rich fine sediment of the Cambrian Yuertus Formation was deposited in the anoxic-suboxidized restricted gulf lagoon environment, and its formation was controlled by high paleoproductivity and poor oxygen exchange jointly, then a shallow-water overlapping sedimentary model has been established. The results will help enrich and improve the sedimentary theory of organic-rich fine sediments.

Cite this article

Zhimin JIN , Xiucheng TAN , Hao TANG , Anjiang SHEN , Zhanfeng QIAO , Jianfeng ZHENG , Fei LI , Shixuan ZHANG , Lei CHEN , Chenggang ZHOU . Sedimentary environment and petrological features of organic-rich fine sediments in shallow water overlapping deposits: A case study of Cambrian Yuertus Formation in northwestern Tarim Basin, NW China[J]. Petroleum Exploration and Development, 2020 , 47(3) : 513 -526 . DOI: 10.1016/S1876-3804(20)60069-6

References

[1] POLLASTRO R M. Total petroleum system assessment of undiscovered resources in the giant Barnett Shale continuous (unconventional) gas accumulation, Fort Worth Basin, Texas. AAPG Bulletin, 2007,91(4):551-578.
[2] CHEN L, LU Y, JIANG S, et al. Heterogeneity of the Lower Silurian Longmaxi marine shale in the southeast Sichuan Basin of China. Marine and Petroleum Geology, 2015,65:232-246.
[3] GHADEER S G, MACQUAKER J H S. Sediment transport processes in an ancient mud-dominated succession: A comparison of processes operating in marine offshore settings and anoxic basinal environments. Journal of the Geological Society, 2011,168(5):1121-1132.
[4] APLIN A C, MACQUAKER J H S. Mudstone diversity: Origin and implications for source, seal, and reservoir properties in petroleum systems. AAPG Bulletin, 2011,95(12):2031-2059.
[5] PLINT A G. Mud dispersal across a Cretaceous prodelta: Storm- generated, wave-enhanced sediment gravity flows inferred from mudstone microtexture and microfacies. Sedimentology, 2014,61(3):609-647.
[6] LAZAR O R, BOHACS K M, MACQUAKER J H S, et al. Capturing key attributes of fine-grained sedimentary rocks in outcrops, cores, and thin sections: Nomenclature and description guidelines. Journal of Sedimentary Research, 2015,85(3):230-246.
[7] JIANG Zaixing, LIANG Chao, WU Jing, et al. Several issues in sedimentological studies on hydrocarbon-bearing fine- grained sedimentary rocks. Acta Petrolei Sinica, 2013,34(6):1031-1039.
[8] BLATT H, MIDDLETON G V, MURRAY R C. Origin of sedimentary rocks. Soil Science, 1973,115(5):400.
[9] KOHL D, SLINGERLAND R, ARTHUR M, et al. Sequence stratigraphy and depositional environments of the Shamokin(Union Springs) Member, Marcellus Formation, and associated strata in the Middle Appalachian Basin. AAPG Bulletin, 2014,98:483-513.
[10] SCHIEBER J, MAKINO Y, KUEHL S A. Evidence for high-energy events and shallow-water deposition in the Chattanooga Shale, Devonian, central Tennessee, USA. Sedimentary Geology, 1994,93(3/4):193-208.
[11] MACQUAKER J H S, BOHACS K M. On the accumulation of mud. Science, 2007,318(5857):1734-1735.
[12] GHADEER S G, MACQUKER J H S. The role of event beds in the preservation of organic carbon in fine-grained sediments: Analyses of the sedimentological processes operating during deposition of the Whitby Mudstone Formation (Toarcian, Lower Jurassic) preserved in northeast England. Marine and Petroleum Geology, 2012,35(1):309-320.
[13] DAVIES R J, CLARKW I R. Submarine slope failure primed and triggered by silica and its diagenesis. Basin Research, 2010,18(3):339-350.
[14] MACQUAKER J H S, BENTLEY S J, BOHACS K M. Wave-enhanced sediment-gravity flows and mud dispersal across continental shelves: Reappraising sediment transport processes operating in ancient mudstone successions. Geology, 2010,38(10):947-950.
[15] CURRAN K J, HILL P S, MILLIGAN T G. Fine-grained suspended sediment dynamics in the Eel River flood plume. Continental Shelf Research, 2002,22(17):2537-2550.
[16] CURRAN K J, HILL P S, SCHELL T M, et al, Inferring the mass fraction of floc-deposited mud: Application to fine- grained turbidites. Sedimentology, 2010,51(5):927-944.
[17] WILSON R D, SCHIEBER J. Muddy prodeltaic hyperpycnites in the Lower Genesee Group of central New York, USA: Implications for mud transport in epicontinental seas. Journal of Sedimentary Research, 2014,84(10):866-874.
[18] SMITH L B, SCHIEBER J, WILSON R D. Shallow-water onlap model for the deposition of Devonian black shales in New York, USA. Geology, 2019,47(3):279-283.
[19] ZHAO Jingzhou. Evoluation on the Cambrian-Ordovician marine source rocks from the north Tarim Basin. Acta Sedimentologica Sinica, 2001,19(1):117-124.
[20] ZHANG S, HUANG H, SU J, et al, Geochemistry of Paleozoic marine oils from the Tarim Basin, NW China. Part 4: Paleobiodegradation and oil charge mixing. Organic Geochemistry, 2014,67(1):41-57.
[21] GU Yi, SHAO Zhibing, CHEN Qianglu, et al. Oil mixgration and accumulation patrern in the Tahe oilfield. Petroleum Geology & Experiment, 2007,29(3):224-230.
[22] SUN Xingli, CHEN Jianfa, LIU Wenhui, et al. Geochemical characteristics of cherts of Lower Cambrian in the Tarim Basin and its implication for environment. Petroleum Exploration and Development, 2004,31(3):45-48.
[23] YU Bingsong, CHEN Jianqiang, LI Xingwu, et al. Rare earth and trace element patterns in bedded-cherts from the bottom of the Lower Cambrian in the Northern Tarim Basin, Northwest China: Implication for depositional environments. Acta Sedimentologica Sinica, 2004,22(1):59-66.
[24] CHEN Qianglu, CHU Chenglin, HU Guang, et al. Sedimentary characteristics and depositional environment of Yuertusi Formation in Keping area, Tarim Basin. Petroleum Geology & Experiment, 2017,39(3):311-317.
[25] ZHAO Zongjv, LUO Jiahong, ZHANG Yunbo, et al. Lithofacies paleogergraphy of Cambrian sequences in the Tarim Basin. Acta Perolei Sinica, 2011,32(6):937-948.
[26] YANG Chengyu, LI Meijun, NI Zhiyong, et al. Siliceous rock origin and significance in the uyirtus formation northwestern margin of Tarim Basin. Acta Sedimentologica Sinica, 2016,34(4):653-661.
[27] ZHANG Min, ZHANG Zhili, YU Shenyang, et al. Carbonate microfacies and encironental parameters of the lower cambrian in the Aksu-Wushi region, Northwest Tarim, Northwest China. Acta Micropalaeontologica Sinica, 2016,33(2):190-200.
[28] TUO J, PHILP R P. Occurrence and distribution of high molecular weight hydrocarbons in selected non-marine source rocks from the Liaohe, Qaidam and Tarim Basins, China. Organic Geochemistry, 2003,34(11):1543-1558.
[29] SAFONOVA I Y, SANTOSH M. Accretionary complexes in the Asia-Pacific region: Tracing archives of ocean plate stratigraphy and tracking mantle plumes. Gondwana Research, 2014,25(1):126-158.
[30] LI Jianghai, ZHOU Xiaobei, LI Weibo, et al. Preliminary reconstruction of tectonic paleogeography of Tarim Basin and its adjacent aeras from Cambrian to Triassic, NW China. Geological Review, 2015,61(6):1225-1234.
[31] FENG Zengzhao, BAO Zhidong, WU Maobing, et al. Lithofacies palaeogeography of the Cambrian in Tarim area. Journal of palaeogeography, 2006,8(4):427-439.
[32] STEINER M, WALLIS E, ERDTMANN B D, et al. Submarine-hydrothermal exhalative ore layers in black shales from South China and associated fossils: Insights into a Lower Cambrian facies and bio-evolution. Palaeogeography Palaeoclimatology Palaeoecology, 2001,169(3):165-191.
[33] XIONG Ran, ZHOU Jingao, NI Xinfeng, et al. Distribution prediction of Lower Cambrian Yuertusi Formation source rocks and its significance to oil and gas exploration in the Tarim Basin. Natural Gas Industry, 2015,35(10):49-56.
[34] ZHOU Zhiyi, ZHAO Zhixin, HU Zhaoxun, et al. Stratigraphy of Tarim Basin. Beijing: Science Press, 2001.
[35] WU Lin, GUAN Shuwei, REN Rong, et al. The characteristics of Precambrian sedimentary basin and the distribution of deep source rock: A case study of Tarim Basin in Neoproterozoic and source rocks in Early Cambrian, Western China. Petroleum Exploration and Development, 2016,43(6):905-915.
[36] ZHANG W, GUAN P, JIAN X, et al. In situ geochemistry of Lower Paleozoic dolomites in the northwestern Tarim basin: Implications for the nature, origin, and evolution of diagenetic fluids. Geochemistry Geophysics Geosystems, 2015,15(7):2744-2764.
[37] YANG Zongyu, LUO Ping, LIU Bo, et al. Analysis of petrological characteristics and origin of siliceous rocks during the earliest Cambrian Yurtus Formation in the Aksu area of the Tarim Basin in Northwest China. Earth Science Frontiers, 2017,24(5):245-264.
[38] HU Guang, LIU Wenhui, TENG Geer, et al. Tectonic-sedimentary constrains for hydrocarbon generating organism assemblage in the Lower Cambrian argillaceous source rocks, Tarim Basin. Oil & Gas Geology, 2014,35(5):685-695.
[39] ZHU Guangyou, CHEN Feiran, CHEN Zhiyong, et al. Discovery and basic characteristics of the high-quality source rocksof the Cambrian Yuertusi Formation in Tarim Basin. Natural Gas Geoscience, 2016,27(1):8-21.
[40] ZHANG Jing, ZHANG Baomin, SHAN Xiuqin. Controlling effects of paleo-climate and paleo-ocean on formation of carbonate reservoirs. Petroleum Exploration and Development, 2014,41(1):121-128.
[41] YANG Xin, XU Xuhui, CHEN Qianglu, et al. Palaeotectonics pattern in Pre-Cambrian and its control on the deposition of the Lower Cambrian source rocks in Tarim Basin, NW China. Natural Gas Geoscience, 2014,25(8):1164-1171.
[42] ZHOU X, CHEN D, QING H, et al. Submarine silica-rich hydrothermal activity during the earliest Cambrian in the Tarim Basin, Northwest China. International Geology Review, 2014,56(15):1906-1918.
[43] XIAO D, TAN X, XI A, et al. An inland facies-controlled eogenetic karst of the carbonate reservoir in the Middle Permian Maokou Formation, southern Sichuan Basin, SW China. Marine and Petroleum Geology, 2016,72:218-233.
[44] TAN Xiucheng, XIAO Di, CHEN Jingshan, et al. New advance and enlightenment of eogenetic karstification. Journal of Palaeogeography, 2015,17(4):441-456.
[45] JIN Zhimin, TAN Xiucheng, GUO Rui, et al. Pore structure characteristics and control factors of carbonate reservoirs:the cretaceous Mishrif formation, Halfaya oilfield, Iraq. Acta Sedimentologica Sinica, 2018,36(5):981-986.
[46] ZHONG Y, TAN X, ZHAO L, et al. Identification of facies-controlled eogenetic karstification in the Upper Cretaceous of the Halfaya oilfield and its impact on reservoir capacity. Geological Journal, 2019,54(1):450-465.
[47] ALGEO T J, LYONS T W. Mo-total organic carbon covariation in modern anoxic marine environments: Implications for analysis of paleoredox and paleohydrographic conditions. Paleoceanography, 2006,21(1):1-23.
[48] ALGEO T J, MAYNARD J B. Trace-metal covariation as a guide to water-mass conditions in ancient anoxic marine environments. Geosphere, 2008,4(5):872-887.
[49] TRIBOVILLARD, NICOLAS, ALGEO, et al. Trace metals as paleoredox and paleoproductivity proxies: An update. Chemical Geology, 2006,232(1):12-32.
[50] SAHOO S K, PLANAVSKY N J, KENDALL B, et al. Ocean oxygenation in the wake of the Marinoan glaciation. Nature, 2012,489(7417):546.
[51] ELBAZ-POULICHET F, SEIDEL J L, JéZéQUEL D, et al. Sedimentary record of redox-sensitive elements(U, Mn, Mo) in a transitory anoxic basin(the Thau lagoon, France). Marine Chemistry, 2005,95(3/4):271-281.
[52] ZHANG Shuichang, ZHANG Baomin, BIAN Lizeng, et al. Decelopment constraints of marine source rocks in China. Earth Science Frontiers, 2005,12(3):39-48.
[53] ZHU Chuanling, YAN Hua, YUN Lu, et al. Characteristics of Cambrian source rocks in well XH1, Shaya Uplift, Tarim Basin. Petroleum Geology & Experiment, 2014,36(5):626-632.
[54] ZHENG Y, ANDERSON R F, VAN GEEN A, et al. Authigenic molybdenum formation in marine sediments: A link to pore water sulfide in the Santa Barbara Basin. Geochimica et Cosmochimica Acta, 2000,64(24):4165-4178.
[55] ANDERSON R F, FLEISHER M Q. Uranium precipitation in Black Sea sediments. Berlin: Springer, 1991: 443-458.
[56] ALGEO T J, TRIBOVILLARD N. Environmental analysis of paleoceanographic systems based on Molybdenum-Uranium covariation. Chemical Geology, 2009,268(3):211-225.
[57] BARNES C E, COCHRAN J K. Geochemistry of uranium in Black Sea sediments. Deep Sea Research Part A Oceanographic Research Papers, 1991,38(10):S1237-S1254.
[58] YU B, DONG H, WIDOM E, et al. Geochemistry of basal Cambrian black shales and cherts from the Northern Tarim Basin, Northwest China: Implications for depositional setting and tectonic history. Journal of Asian Earth Sciences, 2009,34(3):418-436.
[59] YAO Chunyan. Stratigraphic geochemistry of the late Ediacaran- Early Cambrian in Akesu-Wushi Area of Xinjiang: Stratigraphic correlation and paleo-enviroment reconstruction. Nanjing: Nanjing University, 2010.
[60] WANG Feiyu, LIU Changwei, ZHU Lei, et al. Study on organic maturity of Cambrian source rocks in Tarim Basin platform area. Xinjiang Petroleum Geology, 2002,23(5):372-375.
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