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    Volume 42 Issue 2
    Feb.  2017
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    Article Navigation >  Earth Science  > 2017  >  42(2): 258-272
    Wei Wei, Zhu Xiaomin, Zhu Shifa, Sun Shuyang, He Mingwei, Yang Dexiang, Wu Jianping, Wang Mingwei, 2017. Origin of Lacustrine Dolomitic Rocks of the Lower Cretaceous Tengge'er Formation in Anan Sag, Erlian Basin. Earth Science, 42(2): 258-272. doi: 10.3799/dqkx.2017.019
    Citation: Wei Wei, Zhu Xiaomin, Zhu Shifa, Sun Shuyang, He Mingwei, Yang Dexiang, Wu Jianping, Wang Mingwei, 2017. Origin of Lacustrine Dolomitic Rocks of the Lower Cretaceous Tengge'er Formation in Anan Sag, Erlian Basin. Earth Science, 42(2): 258-272. doi: 10.3799/dqkx.2017.019
    shu

    Origin of Lacustrine Dolomitic Rocks of the Lower Cretaceous Tengge'er Formation in Anan Sag, Erlian Basin

    doi: 10.3799/dqkx.2017.019
    • 1.

      College of Geosciences, China University of Petroleum, Beijing 102249, China

    • 2.

      State Key Laboratory of Petroleum Resource and Prospecting, China University of Petroleum, Beijing 102249, China

    • 3.

      Research Institute of Petroleum Exploration and Development, Huabei Oilfield Company, PetroChina, Renqiu 062550, China

    • Received Date: 2016-08-05
    • Publish Date: 2017-02-15
      Abstract
    • The Lower Cretaceous source rocks in Anan sag of Erlian basin develop a set of lacustrine fine-grained dolomitic rocks, composed of dolomitic mudstone, dolomitic tuffite, and dolomitic sandstone, which are rich in tight oil. But its petrological characteristics and origin of dolomite are still unclear.Analysis of core observation, thin section, Scanning Electron Microscope (SEM), and geochemical data show the dolomitic rocks mainly include: (1) The subhedral, micritic-powder crystalline dolomite distributing in laminated and star structure dolomitic mudstone and dolomitic tuffite; (2) The euhedral, powder-fine crystalline dolomite distributed massive dolomitic tuffite and dolomitic sandstone. Their mechanisms of dolomitization are different: (1) The subhedral, micritic-powder crystalline dolomite with higher δ13CPDB values (av. 5.4‰), higher δ18CPDB (av. -13‰), and lower fluid inclusion homogenization temperature (50-75 ℃), is dominated by early diagenetic dolomitization associated with methanogenesis. The source of Mg2+ is mainly from alteration of tuffaceous materials. (2) The euhedral, powder-fine crystalline dolomite is characteristic of bigger and finer crystals, lower δ13CPDB values (0.2‰-0.7‰), lower δ18OPDB (av. -19.4‰), and higher fluid inclusion homogenization temperature (about 119 ℃). It is dominated by burial dolomitizationand affected by the controls of methanogenesis anddegradation of organic matter.The source of Mg2+ is mainly from transformation of clay minerals and deep fluid.

       

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    • Alperin, M.J., Reeburgh, W.S., Whiticar, M.J., 1988.Carbon and Hydrogen Isotope Fractionation Resulting from Anaerobic Methane Oxidation.Global Biogeochemical Cycles, 2(3):279-288.doi: 10.1029/gb002i003p00279
      Banner, J.L., Hanson, G.N., 1990.Calculation of Simultaneous Isotopic and Trace Element Variations during Water-Rock Interaction with Applications to Carbonate Diagenesis.Geochimica et Cosmochimica Acta, 54(11):3123-3137.doi: 10.1016/0016-7037(90)90128-8
      Boetius, A., Ravenschlag, K., Schubert, C.J., et al., 2000.A Marine Microbial Consortium Apparently Mediating Anaerobic Oxidation of Methane.Nature, 407(6804):623-626.doi: 10.1038/35036572
      Bonnetti, C., Malartre, F., Huault, V., et al., 2014.Sedimentology, Stratigraphy and Palynological Occurrences of the Late Cretaceous Erlian Formation, Erlian Basin, Inner Mongolia, People's Republic of China.Cretaceous Research, 48:177-192.doi: 10.1016/j.cretres.2013.09.013
      Chen, Z.L., Liu, G.D., Huang, Z.L., et al., 2014.Controls of Oil Family Distribution and Composition in Nonmarine Petroleum Systems:A Case Study from Inner Mongolia Erlian Basin, Northern China.Journal of Asian Earth Sciences, 92:36-52.doi: 10.1016/j.jseaes.2014.06.006
      Deffeyes, K.S., Lucia, F.J., Weyl, P.K., 1965.Dolomitization of Recent and Plio-Pleistocenee Sediments by Marine Evaporate Waters on Bonaire, Netherlands Antilles.In:Pray, L.C., Murray, R.C., eds., Dolomitization and Limestone Diagenesis.SEPM Special Publication, 13:71-88.
      Deng, S.C., Dong, H.L., Guo, L., et al., 2010.Microbial Dolomite Precipitation Using Sulfate Reducing and Halophilic Bacteria:Results from Qinghai Lake, Tibetan Plateau, NW China.Chemical Geology, 278(3-4):151-159.doi: 10.1016/j.chemgeo.2010.09.008
      Epstein, S., Buchsbaum, R., Lowenstam, H.A., et al., 1953.Revised Carbonate-Water Isotopic Temperature Scale.Geological Society of America Bulletin, 64(11):1315-1326.doi: 10.1130/0016-7606(1953)64[1315:rcits]2.0.co;2
      Feng, Y.L., Zhang, Y.J., Wang, R.J., et al., 2011.Dolomites Genesis and Hydrocarbon Enrichment of the Fengcheng Formation in the Northwestern Margin of Junggar Basin.Petroleum Exploration and Development, 38(6):685-692(in Chinese with English abstract). https://www.researchgate.net/publication/281925063_Dolomites_genesis_and_hydrocarbon_enrichment_of_the_Fengcheng_Formation_in_the_northwestern_margin_of_Junggar_Basin_J
      Fronval, T., Jensen, N.B., Buchardt, B., 1995.Oxygen Isotope Disequilibrium Precipitation of Calcite in Lake Arresø, Denmark.Geology, 23(5):463-466.doi:10.1130/0091-7613(1995)023<0463:oidpoc>2.3.co;2
      Games, L.M., HayesRobert, J.M., Gunsalus, P., 1978.Methane-Producing Bacteria:Natural Fractionations of the Stable Carbon Isotopes.Geochimica et Cosmochimica Acta, 42(8):1295-1297.doi: 10.1016/0016-7037(78)90123-0
      Garrels, R.M., Mackenzie, F.T., 1967.Origin of the Chemical Compositions of some Springs and Lakes.Advances in Chemistry, 67:222-242.doi: 10.1021/ba-1967-0067.ch010
      Garrels, R.M., 1967.Genesis of Some Ground Waters from Igneous Rocks.In:Abelson, P.H., ed., Researches in Geochemistry.Wiley, New York, 405-420.
      Gasse, F., Fontes, J.C., Plaziat, J.C., et al., 1987.Biological Remains, Geochemistry and Stable Isotopes for the Reconstruction of Environmental and Hydrological Changes in the Holocene Lakes from North Sahara.Palaeogeography, Palaeoclimatology, Palaeoecology, 60:1-46.doi: 10.1016/0031-0182(87)90022-8
      Guo, J., Zeng, J.H., Song, G.Q., et al., 2014.Characteristics and Origin of Carbonate Cements of Shahejie Formation of Central Uplift Belt in Dongying Depression.Earth Science, 39(5):565-576(in Chinese with English abstract). https://www.researchgate.net/publication/286835446_Characteristics_and_origin_of_carbonate_cements_of_Shahejie_Formation_of_central_uplift_belt_in_Dongying_depression
      Han, X.T., Bao, Z.Y., Xie, S.Y., 2016.Origin and Geochemical Characteristics of Dolomites in the Middle Permian Formation, SW Sichuan Basin, China.Earth Science, 41(1):167-176(in Chinese with English abstract).
      Hu, W.X., Zhu, J.Q., Wang, X.L., et al., 2014.Characteristics, Origin and Geological Implications of the Cambrian Microbial Dolomite in Keping Area, Tarim Basin.Oil & Gas Geology, 35(6):860-869(in Chinese with English abstract).
      Huang, S.J., 2010.Diagenesis of Carbonate Rocks.Geological Publishing House, Beijing (in Chinese).
      Jansa, L.F., Noguera Urrea, V.H., 1990.Geology and Diagenetic History of Overpressured Sandstone Reservoirs, Venture Gas Field, Offshore Nova Scotia, Canada.AAPG Bulletin, 74(10):1640-1658.doi: 10.1306/0c9b2551-1710-11d7-8645000102c1865d
      Jia, G.N., 2012.Study on Stratigraphy and Sedimentary System in the Tenggeer Formation of Anan Sag, Erlian Basin (Dissertation).China University of Geosciences, Beijing.
      Keith, M.L., Weber, J.N., 1964.Carbon and Oxygen Isotopic Composition of Selected Limestones and Fossils.Geochimica et Cosmochimica Acta, 28(10-11):1787-1816.doi: 10.1016/0016-7037(64)90022-5
      Kenward, P.A., Goldstein, R.H., González, L.A., et al., 2009.Precipitation of Low-Temperature Dolomite from an Anaerobic Microbial Consortium:The Role of Methanogenic Archaea.Geobiology, 7(5):556-565.doi: 10.1111/j.1472-4669.2009.00210.x
      Kuang, L.C., Hu, W.X., Wang, X.L., et al., 2013.Research of the Tight Oil Reservoir in the Lucaogou Formation in Jimusar Sag:Analysis of Lithology and Porosity Characteristics.Geological Journal of China Universities, 19(3):529-535(in Chinese with English abstract).
      Kuang, L.C., Tang, Y., Lei, D.W., et al., 2012.Formation Conditions and Exploration Potential of Tight Oil in the Permian Saline Lacustrine Dolomitic Rock, Junggar Basin, NW China.Petroleum Exploration and Development, 39(6):657-667(in Chinese with English abstract). http://www.sciencedirect.com/science/article/pii/S1876380412600950
      Lan, B.F., Yang, K.B., Peng, C.L., et al., 2014.Analysis of the Exploration Potential of Tight Oil in Anan Sag, Erlian Basin.Complex Hydrocarbon Reservoirs, 7(2):9-12(in Chinese with English abstract).
      Land, L.S., 1985.Dolomitization.AAPG-Continuing Education Courses Notes, 24:1-12
      Lei, C., Li, H., Yang, R., et al., 2012.Lacustrine Microbial Dolomite of the Middle Permian Lucaogou Formation in (U) rümqi, Xinjiang.Journal of Palaeogeography, 14(6):767-775(in Chinese with English abstract).
      Li, B., Yan, J.X., Liu, X.T., et al., 2010.The Organogenic Dolomite Model:Mechanism, Progress and Significance.Journal of Palaeogeography, 12(6):699-710(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GDLX201006009.htm
      Li, H., Liu, Y.Q., Li, W.H., et al., 2013.The Microbial Precipitation of Lacustrine Dolomite from Permian Formation, Urumchi, Xinjiang, China.Geological Bulletin of China, 32(4):661-670(in Chinese with English abstract). https://www.researchgate.net/publication/285995607_The_microbial_precipitation_of_lacustrine_dolomite_from_Permian_Formation_Urumchi_Xinjiang_China
      Li, T.T., Zhu, R.K., Bai, B., et al., 2015.Characteristics of Mixed Sedimentary Reservoir:Taking the Lower Cretaceous Mixed Sedimentary Rock of Qingxi Depression in Jiuquan Basin as an Example.Acta Sedimentologica Sinica, 33(2):376-384(in Chinese with English abstract).
      Li, X.Y., Xiao, Y., Yang, Q.F., 2013.Lithologic Reservoir and Tight Oil Exploration Potential in Anan Subsag, Erlian Basin.China Petroleum Exploration, 18(6):56-61(in Chinese with English abstract).
      Lin, C.S., Kenneth, E., Li, S.T., et al., 2001.Sequence Architecture, Depositional Systems, and Controls on Development of Lacustrine Basin Fills in Part of the Erlian Basin, Northeast China.AAPG Bulletin, 85(11):2017-2043.doi: 10.1306/8626D0DB-173B-11D7-8645000102C1865D
      Liu, G., Zhou, D.S., 2007.Application of Microelements Analysis in Identifying Sedimentary Environment-Taking Qianjiang Formation in the Jianghan Basin as an Example.Petroleum Geology & Experiment, 29(3):307-310, 314(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYSD200703016.htm
      Liu, Y.Q., Jiao, X., Li, H., et al., 2011.Primary Dolostone Formation Related to Mantle-Originated Exhalative Hydrothermal Activities, Permian Yuejingou Section, Santanghu Area, Xinjiang, NW China.Science in China (Series D), 41(12):1862-1871(in Chinese). http://www.cnki.com.cn/Article/CJFDTOTAL-JDXG201202002.htm
      Liu, Y.Q., Zhou, D.W., Jiao, X., et al., 2013.A New Type of Sedimentary Rocks:Mantle-Originated Hydroclastites and Hydrothermal Exhalites, Santanghu Area, Xinjiang, NW China.Acta Sedimentologica Sinica, 31(5):773-781(in Chinese with English abstract).
      Luo, P., Yang, S.S., Ma, L., et al., 2001.Origin, Feature and Its Significance to the Petroleum Exploration of the Clay-Size Plagioclase in Lacustrine Laminated Argillaceous Dolomite, Qingxi Depression in Jiuxi Basin.Petroleum Exploration and Development, 28(6):32-33(in Chinese with English abstract). https://www.researchgate.net/publication/298230943_Origin_feature_and_its_significance_to_the_petroleum_exploration_of_the_clay-size_plagioclase_in_lacustrine_laminated_argillaceous_dolomite_Qingxi_depression_in_Jiuxi_basin
      Mattes, B.W., Mountjoy, E.W., 1980.Burial Dolomitization of the Upper Devonian Miette Buildup, Jasper National Park, Alberta.Concepts and Models of Dolomitization, 28:259-297.doi: 10.2110/pec.80.28.0259
      Mazzullo, S.J., 2000.Organogenic Dolomitization in Peritidal to Deep-Sea Sediments.Journal of Sedimentary Research, 70(1):10-23.doi: 10.1306/2dc408f9-0e47-11d7-8643000102c1865d
      Mazzullo, S.J., Bischoff, W.D., Teal, C.S., 1995.Holocene Shallow-Subtidal Dolomitization by Near-Normal Seawater, Northern Belize.Geology, 23(4):341-344.doi:10.1130/0091-7613(1995)023<0341:hssdbn>2.3.co;2
      McKinley, J.M., Worden, R.H., Ruffell, A.H., 2003.Smectite in Sandstones:A Review of the Controls on Occurrence and Behaviour during Diagenesis.International Association of Sedimentologists Special Publications, 34:109-128.doi: 10.1002/9781444304336.ch5
      Roberts, J.A., Bennett, P.C., González, L.A., et al., 2004.Microbial Precipitation of Dolomite in Methanogenic Groundwater.Geology, 32(4):277-280.doi: 10.1130/g20246.2
      Rosenfeld, W.D., Silverman, S.R., 1959.Carbon Isotope Fractionation in Bacterial Production of Methane.Science, 130(3389):1658-1659.doi: 10.1126/science.130.3389.1658-a
      Sánchez-Román, M., Vasconcelos, C., Schmid, T., et al., 2008.Aerobic Microbial Dolomite at the Nanometer Scale:Implications for the Geologic Record.Geology, 36(11):879-882.doi: 10.1130/g25013a.1
      Shackleton, N.J., 1974.Attainment of Isotopic Equilibrium between Ocean Water and the Benthonic Foraminifera Genus Uvigerina:Isotopic Changes in the Ocean during the Last Glacial.Colloques Internationaux du C.N.R.S., 219:203-209.
      Sholkovitz, E.R., Landing, W.M., Lewis, B.L., 1994.Ocean Particle Chemistry:The Fractionation of Rare Earth Elements between Suspended Particles and Seawater.Geochimica et Cosmochimica Acta, 58(6):1567-1579.doi: 10.1016/0016-7037(94)90559-2
      Sun, S.Q., 1994.A Reappraisal of Dolomite Abundance and Occurrence in the Phanerozoic.Journal of Sedimentary Research, 64(2a):396-404.doi: 10.1306/d4267db1-2b26-11d7-8648000102c1865d
      Tan, H.B., Yu, S.S., 1999.Present Situation and Future Development of Elemental Geochemistry in the Study of Lake Sediments' Evolution.Journal of Salt Lake Research, 7(3):58-65(in Chinese with English abstract).
      Teranes, J.L., McKenzie, J.A., Lotter, A.F., et al., 1999.Stable Isotope Response to Lake Eutrophication:Calibration of a High-Resolution Lacustrine Sequence from Baldeggersee, Switzerland.Limnology and Oceanography, 44(2):320-333.doi: 10.4319/lo.1999.44.2.0320
      van Lith, Y.V., Warthmann, R., Vasconcelos, C., et al., 2003.Microbial Fossilization in Carbonate Sediments:A Result of the Bacterial Surface Involvement in Dolomite Precipitation.Sedimentology, 50(2):237-245.doi: 10.1046/j.1365-3091.2003.00550.x
      Vasconcelos, C., Mckenzie, J.A., 1997.Microbial Mediation of Modern Dolomite Precipitation and Diagenesis under Anoxic Conditions (Lagoa Vermelha, Rio de Janeiro, Brazil).Journal of Sedimentary Research, 67(3):378-390.doi: 10.1306/D4268577-2B26-11D7-8648000102C1865D
      Vasconcelos, C., McKenzie, J.A., Bernasconi, S., et al., 1995.Microbial Mediation as a Possible Mechanism for Natural Dolomite Formation at Low Temperatures.Nature, 377(6546):220-222.doi: 10.1038/377220a0
      Wacey, D., Wright, D.T., Boyce, A.J., 2007.A Stable Isotope Study of Microbial Dolomite Formation in the Coorong Region, South Australia.Chemical Geology, 244(1-2):155-174.doi: 10.1016/j.chemgeo.2007.06.032
      Wang, H.L., Gao, X.Z., Yang, D.X., et al., 2014.Distribution Characteristics and Controlling Factors of the Lower Cretaceous Lacustrine Dolomitic Rock in Erlian Basin.Geoscience, 28(1):163-172(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-XDDZ201401017.htm
      Wang, Z.F., Shi, Z.Q., Zhang, D.J., et al., 2015.Microscopic Features and Genesis for Miocene to Pliocene Dolomite in Well Xike-1, Xisha Islands.Earth Science, 40(4):633-644 (in Chinese with English abstract). https://www.researchgate.net/publication/281786711_Microscopic_features_and_genesis_for_miocene_topliocene_dolomite_in_well_Xike-1_Xisha_Islands
      Warthmann, R., van Lith, Y.V., Vasconcelos, C., et al., 2000.Bacterially Induced Dolomite Precipitation in Anoxic Culture Experiments.Geology, 28(12):1091-1094.doi:10.1130/0091-7613(2000)028<1091:bidpia>2.3.co;2
      Wei, W., Zhu, X.M., Guo, D.B., et al., 2015.Carbonate Cements in Lower Cretaceous Bayingebi Sandstone Reservoirs in Chagan Sag, Yin-E Basin:Formation Phases and Formation Mechanisms.Geochimica, 44(6):590-599 (in Chinese with English abstract).
      Whiticar, M.J., 1999.Carbon and Hydrogen Isotope Systematics of Bacterial Formation and Oxidation of Methane.Chemical Geology, 161(1-3):291-314.doi: 10.1016/s0009-2541(99)00092-3
      Yang, W., Wang, Q.H., Liu, X.Z., 2000.Dolomite Origin of Lower Ordovician in Hetian River Gas Field, Tarim Basin.Acta Sedimentologica Sinica, 18(4):544-548(in Chinese with English abstract).
      Yu, B.S., Dong, H.L., Jiang, H.C., et al., 2007.Discovery of Spheric Dolomite Aggregations in Sediments from the Bottom of Qinghai Lake and its Significance for Dolomite Problem.Geoscience, 21(1):66-70(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-XDDZ200701006.htm
      Zenger, D.H., Dunham, J.B., Ethington, R.L., 1980.Concepts and Models of Dolomitization.SEPM, Special Publication, 28:320. http://www.osti.gov/scitech/biblio/6035041
      Zhang, L.P., Wang, D.P., 1994.Palaeoclimatic Ciiaracteristics and Themechanism for Climatic Ciianges in Thesongliao Basin during the Cretaceous.Sedimentary Facies and Palaeogeography, 14(1):11-16 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YXGD401.001.htm
      Zhang, W.C., Zhu, Y.H., Jiang, D.H., et al., 1997.The Law of Oil Controlled by Subsags and Prospect of Petroleum Exploration in Erlian Basin.Acta Petrolei Sinica, 18(4):25-31 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYXB199704004.htm
      Zhang, X.B., Wang, Z.Y., Xu, Y.C., 2000.Finding of the Dolostones with Special Carbon Isotopic Composition and Its Significance.Acta Sedimentologica Sinica, 18(3):449-452(in Chinese with English abstract).
      Zheng, R.C., Wang, C.S., Zhu, L.D., et al., 2003.Discovery of the First Example of "White Smoke Type" of Exhalative Rock (Hydrothermal Sedimentary Dolostone) in Jiuxi Basin and Its Significance.Journal of Chengdu University of Technology, 30(1):1-8(in Chinese with English abstract).
      Zhu, S.F., Zhu, X.M., Liu, Y.H., et al., 2014.Petrological and Geochemical Features of Dolomitic Rocks in the Lower Permian Fengcheng Formation in Wuerhe-Xiazijie Area, Junggar Basin.Geological Review, 60(5):1113-1122 (in Chinese with English abstract).
      Zhu, S.F., Zhu, X.M., Tao, W.F., et al., 2013.Origin of Dolomitic Reservoir Rock in the Permian Fengcheng Formation in Wu-Xia Area of the Junggar Basin.Geological Journal of China Universities, 19(1):38-45(in Chinese with English abstract).
      Zhu, Y.H., Zhang, W.C., Wang, H.S., 2000.Sedimentary Facies and Hydrocarbon-Bearing of Lower Cretaceous Strata in Erlian Basin.Science Press, Beijing, 22-23(in Chinese).
      冯有良, 张义杰, 王瑞菊, 等, 2011.准噶尔盆地西北缘风城组白云岩成因及油气富集因素.石油勘探与开发, 38(6): 685-692. http://www.cnki.com.cn/Article/CJFDTOTAL-SKYK201106006.htm
      郭佳, 曾溅辉, 宋国奇, 等, 2014.东营凹陷中央隆起带沙河街组碳酸盐胶结物发育特征及其形成机制.地球科学, 39(5): 565-576. http://www.earth-science.net/WebPage/Article.aspx?id=2865
      韩晓涛, 鲍征宇, 谢淑云, 2016.四川盆地西南中二叠统白云岩的地球化学特征及其成因.地球科学, 41(1): 167-176. http://www.earth-science.net/WebPage/Article.aspx?id=3229
      胡文瑄, 朱井泉, 王小林, 等, 2014.塔里木盆地柯坪地区寒武系微生物白云岩特征、成因及意义.石油与天然气地质, 35(6): 860-869. http://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201406015.htm
      黄思静, 2010.碳酸盐岩的成岩作用.北京:地质出版社.
      贾国娜, 2012.二连盆地阿南凹陷腾一段层序地层及沉积体系研究(硕士学位论文).北京:中国地质大学.
      匡立春, 胡文瑄, 王绪龙, 等, 2013.吉木萨尔凹陷芦草沟组致密油储层初步研究:岩性与孔隙特征分析.高校地质学报, 19(3): 529-535. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX201303015.htm
      匡立春, 唐勇, 雷德文, 等, 2012.准噶尔盆地二叠系咸化湖相云质岩致密油形成条件与勘探潜力.石油勘探与开发, 39(6): 657-667. http://www.cnki.com.cn/Article/CJFDTOTAL-SKYK201206004.htm
      蓝宝锋, 杨克兵, 彭传利, 等, 2014.二连盆地阿南凹陷致密油勘探潜力分析.复杂油气藏, 7(2): 9-12. http://www.cnki.com.cn/Article/CJFDTOTAL-FZYQ201402003.htm
      雷川, 李红, 杨锐, 等, 2012.新疆乌鲁木齐地区中二叠统芦草沟组湖相微生物成因白云石特征.古地理学报, 14(6): 767-775. http://www.cnki.com.cn/Article/CJFDTOTAL-GDLX201206012.htm
      李波, 颜佳新, 刘喜停, 等, 2010.白云岩有机成因模式:机制、进展与意义.古地理学报, 12(6): 699-710. http://www.cnki.com.cn/Article/CJFDTOTAL-GDLX201006009.htm
      李红, 柳益群, 李文厚, 等, 2013.新疆乌鲁木齐二叠系湖相微生物白云岩成因.地质通报, 32(4): 661-670. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD201304015.htm
      李婷婷, 朱如凯, 白斌, 等, 2015.混积岩储层特征——以酒泉盆地青西凹陷下白垩统混积岩为例.沉积学报, 33(2): 376-384. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201502017.htm
      李秀英, 肖阳, 杨全凤, 2013.二连盆地阿南洼槽岩性油藏及致密油勘探潜力.中国石油勘探, 18(6): 56-61. http://www.cnki.com.cn/Article/CJFDTOTAL-KTSY201306010.htm
      刘刚, 周东升, 2007.微量元素分析在判别沉积环境中的应用——以江汉盆地潜江组为例.石油实验地质, 29(3): 307-310, 314. http://www.cnki.com.cn/Article/CJFDTOTAL-SYSD200703016.htm
      柳益群, 焦鑫, 李红, 等, 2011.新疆三塘湖跃进沟二叠系地幔热液喷流型原生白云岩.中国科学(D辑), 41(12): 1862-1871. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201112015.htm
      柳益群, 周鼎武, 焦鑫, 等, 2013.一类新型沉积岩:地幔热液喷积岩——以中国新疆三塘湖地区为例.沉积学报, 31(5): 773-781. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201305004.htm
      罗平, 杨式升, 马龙, 等, 2001.酒西盆地青西坳陷湖相纹层状泥质白云岩中泥级斜长石成因、特征与油气勘探意义.石油勘探与开发, 28(6): 32-33. http://www.cnki.com.cn/Article/CJFDTOTAL-SKYK200106009.htm
      谭红兵, 于升松, 1999.我国湖泊沉积环境演变研究中元素地球化学的应用现状及发展方向.盐湖研究, 7(3): 58-65. http://www.cnki.com.cn/Article/CJFDTOTAL-YHYJ199903010.htm
      王会来, 高先志, 杨德相, 等, 2014.二连盆地下白垩统湖相云质岩分布及控制因素.现代地质, 28(1): 163-172. http://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ201401017.htm
      王振峰, 时志强, 张道军, 等, 2015.西沙群岛西科1井中新统-上新统白云岩微观特征及成因.地球科学, 40(4): 633-644. http://www.earth-science.net/WebPage/Article.aspx?id=3071
      魏巍, 朱筱敏, 国殿斌, 等, 2015.查干凹陷下白垩统砂岩储层碳酸盐胶结物成岩期次及形成机理.地球化学, 44(6): 590-599. http://www.cnki.com.cn/Article/CJFDTOTAL-DQHX201506008.htm
      杨威, 王清华, 刘效曾, 2000.塔里木盆地和田河气田下奥陶统白云岩成因.沉积学报, 18(4): 544-548. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200004010.htm
      于炳松, 董海良, 蒋宏忱, 等, 2007.青海湖底沉积物中球状白云石集合体的发现及其地质意义.现代地质, 21(1): 66-70. http://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ200701006.htm
      张立平, 王东坡, 1994.松辽盆地白垩纪古气候特征及其变化机制.岩相古地理, 14(1): 11-16. http://www.cnki.com.cn/Article/CJFDTOTAL-YXGD401.001.htm
      张文朝, 祝玉衡, 姜冬华, 等, 1997.二连盆地"洼槽"控油规律与油气勘探前景.石油学报, 18(4): 25-31.
      张晓宝, 王志勇, 徐永昌, 2000.特殊碳同位素组成白云岩的发现及其意义.沉积学报, 18(3): 449-452. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200003020.htm
      郑荣才, 王成善, 朱利东, 等, 2003.酒西盆地首例湖相"白烟型"喷流岩-热水沉积白云岩的发现及其意义.成都理工大学学报(自然科学版), 30(1): 1-8. http://www.cnki.com.cn/Article/CJFDTOTAL-CDLG200301000.htm
      朱世发, 朱筱敏, 刘英辉, 等, 2014.准噶尔盆地西北缘北东段下二叠统风城组白云质岩岩石学和岩石地球化学特征.地质论评, 60(5): 1113-1122. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP201405018.htm
      朱世发, 朱筱敏, 陶文芳, 等, 2013.准噶尔盆地乌夏地区二叠系风城组云质岩类成因研究.高校地质学报, 19(1): 38-45. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX201301006.htm
      祝玉衡, 张文朝, 王洪生, 2000.二连盆地下白垩统沉积相及含油性.北京:科学出版社, 22-23.
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