Features and Model of Mixed Sediments in Lower Submember of First Member of Shahejie Formation in Lixian Slope, Raoyang Sag
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摘要: 混积滩坝不仅发育于海相沉积盆地，也广泛发育于陆相断陷湖盆，特别是在缓坡带最为发育并与油气富集密切相关.以饶阳凹陷蠡县斜坡为靶区，基于岩心与测井资料，通过岩心与薄片观察、粒度分析、微量元素含量测定等手段确定了研究区沙一下亚段混积滩坝沉积和分布特征，建立了断陷湖盆缓坡混积滩坝的沉积模式.研究表明，可以依据岩性将蠡县斜坡发育的滩坝分为碎屑岩滩坝、碳酸盐岩滩坝和混积滩坝，其中混积滩坝又可以分为成分混积滩坝和层系混积滩坝.混积滩坝岩性以灰质砂岩、砂质鲕粒灰岩、生物碎屑灰岩等为主，其发育与展布受控于古气候、古物源、古地貌、古水体等地质因素，在斜坡不同位置、不同沉积阶段构成了不同类型的滩坝沉积组合.斜坡近岸缓坡带发育层系混积滩坝以及碎屑岩滩坝，远岸缓坡带发育成分混积滩坝，远岸水下低隆带主要发育碳酸盐岩滩坝.Abstract: Not only are mixed rocks distributed in marine basins,but they are also distributed in a large number of hanging wall slope areas in rift sags and related to hydrocarbon accumulation closely. Mainly based on the core data and logging data of the Lixian slope,and the sedimentary characteristics and distribution of mixed beach-bars are studied through the core and thin section observation,grain size analysis,log facies analysis. Firstly,seismic data,pollen data,and trace element data were analyzed to restore the depositional environment controlling factors such as paleoclimate,paleo-provenance,paleogeomorphology,and paleo-water characteristics in the first member of Shahejie Formation. Then,the sedimentary model of the mixed beach-bars in the lower submember of the first member of Shahejie Formation in Lixian slope was systematically built. The results show that the beach-bar facies developed in the hanging wall slope area of Raoyang sag can be divided into siliciclastic beach-bars,carbonate beach-bars,and mixed beach-bars according to petrologic characteristics. Moreover,mixed beach-bars can be divided into component-mixed beach-bars and stratified-mixed beach-bars. The lithology of mixed beach-bar was mainly of calcareous sandstone,sandy oolitic limestone,and bioclastic limestone. The distribution of mixed beach-bar was controlled by factors such as paleoclimate,paleo-provenance,paleogeomorphology,and paleo-water characteristics. Therefore,different sedimentary patterns developed in different positions and different sedimentary stages on the slope. Stratified-mixed beach-bars and siliciclastic beach-bars were deposited in the near-shore ramp,and component-mixed beach-bars were deposited in the far-shore ramp. Carbonate beach-bars were mainly distributed on the far-shore low uplift.
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图 1 饶阳凹陷蠡县斜坡构造位置及地层发育剖面
Fig. 1. Structural map and generalized stratigraphic profile of Lixian slope
图 2 饶阳凹陷蠡县斜坡沙一下亚段特殊岩性段沉积相平面展布
Fig. 2. Distribution of beach-bar sandbodies and mixed rocks of the 1st member of Shahejie Formation, Lixian slope, Raoyang sag
图 3 饶阳凹陷蠡县斜坡沙一段滩坝沉积典型井单井柱状图
a.高31井单井柱状图；b.西柳4井单井柱状图；c.宁55井单井柱状图；d.饶3井单井柱状图
Fig. 3. Sedimentary facies of wells G31, XL4, N55 and Rao3
图 4 饶阳凹陷蠡县斜坡沙一段滩坝沉积典型岩性照片
a.灰白色粉细砂岩, 小型楔状交错层理, 高15井, 2 351.80 m；b.灰色泥质粉砂岩，波状交错层理, 高22井, 2 951.20 m；c.灰白色细砂岩, 浪成砂纹交错层理, 西柳16X井, 3 094.10 m；d.灰黑色灰质页岩, 水平层理, 高52井, 3 095.40 m；e.灰色含鲕粒细砂岩, 饶4井, 3 409.70 m；f.灰白色鲕粒灰岩, 高31井, 2 470.40 m；g.灰白色泥质粉砂岩, 含大量植物碎屑, 雁61井, 2 732.70 m；h.生物碎屑灰岩, 饶3井, 2 797.20 m；i.灰白色颗粒灰岩, 饶3井, 2 797.30 m
Fig. 4. Typical core photos of the 1st member of Shahejie Formation, Lixian slope, Raoyang sag
图 5 饶阳凹陷蠡县斜坡沙一段滩坝沉积镜下特征
a.灰质页岩；高保1X井，2 333.10 m，单偏光，20x；b.灰质页岩，高保1X井，2 333.70 m，单偏光，100x；c.粉砂质泥岩；宁49井，3 296.60 m，单偏光，50x；d.钙质粉细砂岩，饶3井，2 793.50 m，单偏光，50x；e.细砂岩；保深3井，2 175.40 m，单偏光，50x；f.灰质粉细砂岩，宁202井，3 571.60 m，单偏光，100x；g.钙质粉细砂岩，饶3井，2 793.50 m，正交光，50x；h.细砂岩，保深3井，2 175.40 m；正交光，50x；i.灰质粉细砂岩，宁202井，3 571.60 m，正交光，100x；j.鲕粒灰岩，西柳4井，3 297.20 m，单偏光，20x；k.砂质鲕粒灰岩，饶3井，2 797.50 m，单偏光，50x；l.复鲕，饶3井，2 800.00 m，单偏光，50x；m.颗粒灰岩，饶3井，2 797.60 m，单偏光，50x；n.颗粒灰岩，饶3井，2 797.60 m，正交光，50x；o.生物碎屑灰岩，饶3井，2 798.20 m，单偏光，100x
Fig. 5. Slice photos of beach-bar sandbodies of the 1st member of Shahejie Formation, Lixian Slope, Raoyang sag
图 6 饶阳凹陷蠡县斜坡沙一段滩坝沉积粒度分析结果
a.保深2井，2 679.00 m；b.保深2井，2 680.00 m；c.宁202井，3 568.80 m；d.宁202井，3 571.60 m；e.饶3井，2 793.50 m；f.饶3井，2 795.20 m
Fig. 6. Main types of grain size probability curves of beach-bar sandbodies of the 1st member of Shahejie Formation, Lixian slope, Raoyang sag
图 7 饶阳凹陷蠡县斜坡沙河街组一段下亚段古物源与滩坝分布叠合
Fig. 7. Distribution of provenance of the lower submember of Shahejie Formation in Lixian slope, Raoyang sag
图 9 饶阳凹陷蠡县斜坡沙河街组一段下亚段古水深分布
古水深分布修改自殷杰等(2017)
Fig. 9. The distribution of water depth of the lower submember of Shahejie Formation in Lixian slope, Raoyang sag
图 10 饶阳凹陷缓坡带沙一段高水位时期沉积模式
Fig. 10. Sedimentary models of beach-bar sandbodies and mixed rocks with high-water level, Lixian slope, Raoyang sag
图 11 饶阳凹陷缓坡带沙一段低水位时期沉积模式
Fig. 11. Sedimentary models of beach-bar sandbodies and mixed rocks with low-water level, Lixian slope, Raoyang sag
表 1 二端元混积岩分类
Table 1. Classification of mixed rocks
类别 组分比例 组分名称 以碳酸盐为主 10% < LS < 25% 含陆源碎屑-碳酸盐岩，如：含砂鲕粒灰岩 25% < LS < 50% 陆源碎屑质-碳酸盐岩，如：砂质鲕粒灰岩 以陆源碎屑为主 TS < 25% 含碳酸盐-陆源碎屑岩，如：含鲕粒砂岩 25% < TS < 50% 碳酸盐质-陆源碎屑岩，如：鲕粒质砂岩 注：TS代表碳酸盐组分；LS代表陆源碎屑组分.修改自董桂玉等(2007). 
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表 2 饶阳凹陷蠡县斜坡沙一段滩坝沉积微量元素含量数据
Table 2. Analysis of the test results of trace elements of the 1st member of Shahejie Formation, Lixian slope, Raoyang sag
井号 样品深度(m) Cu(μg/g) Sr(μg/g) Ba(μg/g) Sr/Cu Sr/Ba 保深3井 2 086.10 62.0 519 977 8.370 968 0.531 218 高36井 2 776.20 59.2 420 441 7.094 595 0.952 381 高52井 3 094.30 54.1 948 861 17.523 110 1.101 045 宁202井 3 465.50 57.2 301 673 5.262 238 0.447 251 宁202井 3 566.70 57.5 762 1 045 13.252 170 0.729 187 宁49井 3 292.30 77.0 277 502 3.597 403 0.551 793 宁49井 3 293.10 61.6 244 386 3.961 039 0.632 124 饶3井 2 792.80 69.3 282 559 4.069 264 0.504 472 饶3井 2 797.00 61.2 366 721 5.980 392 0.507 628 饶4井 3 406.94 74.4 406 630 5.456 989 0.644 444 饶4井 3 410.86 80.7 340 580 4.213 135 0.586 207 任3井 2 771.40 70.5 288 517 4.085 106 0.557 060 任3井 2 785.80 73.7 212 541 2.876 526 0.391 867 西柳5井 3 330.34 42.4 692 799 16.320 750 0.866 083 西柳5井 3 324.24 67.8 470 713 6.932 153 0.659 187
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[1] Chen, H.H., Zhu, X.M., Huang, H.D., et al., 2017. Sediment Provenance of Shahejie Formation in Lixian Slope of Raoyang Depression Based on the Detrital Zircon Dating Analysis. Earth Science, 42(11): 1955-1971(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201711008 [2] Chen, H.H., Zhu, X.M., Wood, L.J., et al., 2019. Evolution of Drainage, Sediment‐Flux and Fluvio‐Deltaic Sedimentary Systems Response in Hanging Wall Depocentres in Evolving Non‐Marine Rift Basins: Paleogene of Raoyang Sag, Bohai Bay Basin, China. Basin Research, 32(1): 116-145. https://doi.org/10.1111/bre.12371 [3] Chen, H.L., Wang, Z.F., Wang, W., et al., 2013. The Mixed Sedimentary Characteristics of Cretaceous Aption of Kashkari Oilfield in Afghanistan. Journal of Oil and Gas Technology, 35(11): 11-14(in Chinese with English abstract). [4] Dong, G.Y., He, Y.B., Chen, H.D., et al., 2007. Mixed Sedimentation of Carbonates of Lagoonal Facies and Terrigenous Clastics of the Middle Submember of Member 1 of Shahejie Formation in Huimin Sag: Taking Shanghe Area in Shandong Province for an Example. Acta Sedimentologica Sinica, 25(3): 343-350(in Chinesewith English abstract). [5] Dong, Y.L., Zhu, X.M., Hua, S.J., et al., 2011. Genetic Types and Evolutionary Model of Mixed Clastic-Carbonate Deposits in the Lower Part of the Sha-1 Formation, the Huanghua Depression. Oil & Gas Geology, 32(1): 98-107(in Chinese with English abstract). [6] Feng, J. L., Cao, J., Hu, K., et al., 2013. Dissolution and Its Impacts on Reservoir Formation in Moderately to Deeply Buried Strata of Mixed Siliciclastic-Carbonate Sediments, Northwestern Qaidam Basin, Northwest China. Marine and Petroleum Geology, 39(1): 124-137. https://doi.org/10.1016/j.marpetgeo.2012.09.002 [7] Jia, Y.Y., Xing, X.J., Sun, G.Q., et al., 2015. The Paleogene-Neogene Paleoclimate Evolution in Western Sector of Northern Margin of Qaidam Basin. Earth Science, 40(12): 1955-1967(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201512002 [8] Jiang, Z.X., Liu, H., Zhang, S.W., et al., 2011. Sedimentary Characteristics of Large-Scale Lacustrine Beach-Bars and Their Formation in the Eocene Boxing Sag of Bohai Bay Basin, East China. Sedimentology, 58(5): 1087-1112. https://doi.org/10.1111/j.1365-3091.2010.01196.x [9] Li, H., Lu, J.L., Li, R.L., et al., 2017. Generation Paleoenvironment and Its Controlling Factors of Lower Cretaceous Lacustrine Hydrocarbon Source Rocks in Changling Depression, South Songliao Basin. Earth Science, 42(10): 1774-1786(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201710012 [10] Li, S. J., Zheng, D. S., Jiang, Z. X., et al., 2005. Water Depth of Paleo-Lacustrine Basin Recovered by Dominance Diversity of Ostracoda: An Example from Sedimentary Period of the Member 3 of Shahejie Formation of Paleogene in Dongying Sag, Shandong Province. Journal of Paleogeography, 7(3): 399-404(in Chinese with English abstract). [11] 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): 307-314(in Chinese with English abstract). [12] Liu, S.Q., 2018, Sedimentary Characteristics of Lacustrine Carbonates in the Upper Fourth Member of Shahejie Formation (Es4s), Western Dongying Depression (Dissertation). China University of Geosciences, Beijing(in Chinese with English abstract). [13] Luo, N.N., Hou, S.T., Ji, Y.L., et al., 2019. Sedimentary Model of Mixed Rocks in Es3s of Paleogene in the Dawangzhuang Area, Raoyang Sag, Bohai Bay Basin. Acta Sedimentologica Sinica. https://doi.org/10.14027/j.issn.1000-0550.2019.096 (in Chinese with English abstract). [14] Luo, S.S., Liu, K.Y., He, Y.B., et al., 2004. Mixed Sedimentary Characteristics and Mode of Terrigenous Clastics and Carbonate in Es4 of Bonan Depression. Journal of Jianghan Petroleum Institute, 26(4): 19-21(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=jhsyxyxb200404005 [15] Ma, H.Y., Yah, B.Y., Yu, P.F., et al., 2013. Carbonate Sedimentary Reservoir Features of Lower Submember of First Member of Shahejie Formation in Central Lixian Slope, Raoyang Sag. China Petroleum Exploration, 18(6): 25-33(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgsykt201306005 [16] Ma, Y.S., Zhao, X., Zhao, X.T., et al., 2007. The Cenozoic Rifting and Uplifting Process on the Southern Margin of Taihangshan Uplift. Acta Geoscientica Sinica, 28(3): 219-233(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqxb200703001 [17] Mount, J.F., 1984. Mixing of Siliciclastic and Carbonate Sediments in Shallow Shelf Environments. Geology, 12(7): 432-435. https://doi.org/10.1130/0091-7613(1984)12432:MOSACS > 2.0.CO; 2 doi: 10.1130/0091-7613(1984)12432:MOSACS>2.0.CO;2 [18] Ren, Y., Zhong, D.K., Liu, H.L., et al., 2018. Isotopic and Elemental Evidence for Paleoenvironmental Evolution of Cambrian Stage 4 Longwangmiao Formation, East Chongqing, China. Earth Science, 43(11):4066-4095(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201811023 [19] Sha, Q.A., 2001. Discussion on Mixing Deposit and Hunji Rock. Journal of Palaeogeography, 3(3): 63-66(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gdlxb200103008 [20] Song, G.Q., Wang, Y.Z., Shi, X.H., et al., 2013. Palaeosalinity and Its Controlling on the Development of Beach and Bar in Lake Facies. Journal of Southwest Petroleum Institute, 35(2): 8-14(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xnsyxyxb201302002 [21] Song, L.J., Liu, C.Y., Zhao, H.G., et al., 2016. Geochemical Characteristics, Sedimentary Environment and Tectonic Setting of Huangqikou Formation, Ordos Basin. Earth Science, 41(8): 1295-1308, 1321(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201608004 [22] Song, M.S., 2005. Sedimentary Environment Geochemistry in the Shasi Section of Southern Ramp, Dongying Depression. Journal of Mineralogy and Petrology, 25(1): 67-73(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kwys200501013 [23] Su, X., Ding, X., Jiang, Z.X., et al., 2012. Using of Multi-microfossil Proxies for Reconstructing Quantitative Paleo-Water Depth during the Deposit Period of LST of Es4s in Dongying Depression. Earth Science Frontiers, 19(1): 188-199(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy201201025 [24] Wang, Q.B., Liu, L., Niu, C.M., et al., 2018. Impacts of the Freshwater Diagenetic Environment to the Mix-Deposition of Lacustrine Carbonate and Clastic at the Steep Slope of Shijiutuo Uplift, Bohai Bay Basin. Earth Science, 43(Suppl.2): 234-242(in Chinese with English abstract). [25] Wen, H. G., Zheng, R. C., Tang, F., et al., 2008. Reconstruction and Analysis of Paleosalanity and Paleoenvironment of the Chang 6 Member in the Gengwan Region, Ordos Basin. Journal of Mineralogy and Petrology, 28(01):114-120(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kwys200801016 [26] Xie, X.N., Ye, M.S., Xu, C.G., et al., 2018. High Quality Reservoirs Characteristics and Forming Mechanisms of Mixed Siliciclastic-Carbonate Sediments in the Bozhong Sag, Bohai Bay Basin. Earth Science, 43(10):3526-3539(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201810015 [27] Yang, C.Q., Sha, Q.A., 1990. Sedimentary Environment of the Middle Devonian Qujing Formation, Qujing, Yunnan Province: A Kind of Mixing Sedimentation of Terrigenous Clastics and Carbonate. Acta Sedimentologica Sinica, 8(2): 59-66(in Chinese with English abstract). [28] Ye, L., Zhu, X.M., Zhang, R.F., et al., 2020. Sediment Environment of Shallow-Water Delta and Beach-Bar of the Member 1 of Shahejie Formation in Lixian Slope of Raoyang Sag, Jizhong Depression. Journal of Palaeogeography, 22(3):587-600(in Chinese with English abstract). [29] Yin, J., Wang, Q., Hao, F., et al., 2017. Palaeolake Environment and Depositional Model of Source Rocks of the Lower Submember of Sha1 in Raoyang Sag, Bohai Bay Basin. Earth Science, 42(7): 1209-1222(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201707016 [30] Zhang, X.H., 2000. Classification and Origin of Mixosedimentite. Geological Science and Technology Information. 19(4): 32-34(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzkjqb200004006 [31] Zhao, X.Z., Lu, X.J., Cui, Z.Q., et al., 2012. Detailed Research of Fine Sequence Stratigraphy and Exploration Results in the Slope Zone of Faulted Basin. Earth Science Frontiers, 19(1): 10-19(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy201201003 [32] Zhao, Z.Y., Zhao, J.H., Wang, H.J., et al., 2007. Distribution Characteristics and Applications of Trace Elements in Junggar Basin. Natural Gas Exploration and Development, 30(2): 30-32, 40(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=trqktykf200702007 [33] Zhu, X.M., Tan, M.X., Dong, Y.L., et al., 2019. Current Hot Topics of Sedimentology: Comment on the 20th International Sedimentological Congress. Acta Sedimentologica Sinica, 37(1): 1-16(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-CJXB201901001.htm [34] Zhu, X.M., Xin, Q.L., Zhang, J.R., et al., 1994. Sedimentary Characteristics and Models of the Beach-Bar Reservoirs in Faulted down Lacustrine Basins. Acta Sedimentologica Sinica, 12(2): 20-28(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199400005184 [35] 陈贺贺, 朱筱敏, 黄捍东, 等, 2017.基于碎屑锆石定年的饶阳凹陷蠡县斜坡沙河街组物源分析.地球科学, 42(11): 1955-1971. doi: 10.3799/dqkx.2017.124 [36] 陈怀龙, 王兆峰, 汪文, 等, 2013.阿富汗喀什喀里油田下白垩统阿普第阶地层混合沉积特征研究.石油天然气学报, 35(11): 11-14. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=jhsyxyxb201311003 [37] 董桂玉, 何幼斌, 陈洪德, 等, 2007.惠民凹陷沙一中湖相碳酸盐与陆源碎屑混合沉积——以山东商河地区为例.沉积学报, 25(3):343-350. [38] 董艳蕾, 朱筱敏, 滑双君, 等, 2011.黄骅坳陷沙河街组一段下亚段混合沉积成因类型及演化模式.石油与天然气地质, 32(1): 98-107. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=syytrqdz201101012 [39] 贾艳艳, 邢学军, 孙国强, 等, 2015.柴北缘西段古-新近纪古气候演化.地球科学, 40(12): 1955-1967. doi: 10.3799/dqkx.2015.176 [40] 李浩, 陆建林, 李瑞磊, 等, 2017.长岭断陷下白垩统湖相烃源岩形成古环境及主控因素.地球科学, 42(10): 1774-1786. doi: 10.3799/dqkx.2017.539 [41] 李守军, 郑德顺, 姜在兴, 等, 2005.用介形类优势分异度恢复古湖盆的水深——以山东东营凹陷古近系沙河街组沙三段湖盆为例.古地理学报, 7(03):399-404. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gdlxb200503010 [42] 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):307-314. [43] 刘圣乾, 2018.东营凹陷西部沙四上亚段湖相碳酸盐岩沉积特征研究(博士学位论文).北京: 中国地质大学. [44] 罗妮娜, 侯守探, 纪友亮, 等, 2019.渤海湾盆地饶阳凹陷大王庄地区古近系沙三上亚段混积模式研究.沉积学报.https://doi.org/10.14027/j.issn.1000-0550.2019.096. [45] 罗顺社, 刘魁元, 何幼斌, 等, 2004.渤南洼陷沙四段陆源碎屑与碳酸盐混合沉积特征与模式.江汉石油学院学报, 26(4):19-21. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=jhsyxyxb200404006 [46] 马红岩, 闫宝义, 于培峰, 等, 2013.饶阳凹陷蠡县斜坡中部沙一下亚段碳酸盐岩沉积储层及油藏特征.中国石油勘探, 18(6): 25-33. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgsykt201306005 [47] 马寅生, 赵逊, 赵希涛, 等, 2007.太行山南缘新生代的隆升与断陷过程.地球学报, 28(3): 219-233. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqxb200703001 [48] 任影, 钟大康, 柳慧琳, 等, 2018.渝东地区寒武系第四阶龙王庙组古环境演化的稳定同位素与主、微量元素证据.地球科学, 43(11):4066-4095. doi: 10.3799/dqkx.2017.590 [49] 沙庆安, 2001.混合沉积和混积岩的讨论.古地理学报, 3(3): 63-66. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gdlxb200103008 [50] 宋国奇, 王延章, 石小虎, 等, 2013.东营沙四段古盐度对碳酸盐岩沉积的控制作用.西南石油大学学报, 35(2): 8-14. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xnsyxyxb201302002 [51] 宋立军, 刘池阳, 赵红格, 等, 2016.鄂尔多斯地区黄旗口组地球化学特征及其沉积环境与构造背景.地球科学, 41(8): 1295-1308, 1321. doi: 10.3799/dqkx.2017.590 [52] 宋明水, 2005.东营凹陷南斜坡沙四段沉积环境的地球化学特征.矿物岩石, 25(1): 67-73. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kwys200501013 [53] 苏新, 丁旋, 姜在兴, 等, 2012.用微体古生物定量水深法对东营凹陷沙四上亚段沉积早期湖泊水深再造.地学前缘, 19(1): 188-199. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy201201025 [54] 王清斌, 刘立, 牛成民, 等, 2018.石臼坨凸起陡坡带大气淡水成岩环境对湖相混积岩储层的影响.地球科学, 43(增刊2): 234-242. doi: 10.3799/dqkx.2018.138 [55] 文华国, 郑荣才, 唐飞, 等, 2008.鄂尔多斯盆地耿湾地区长6段古盐度恢复与古环境分析.矿物岩石, 28(1):114-120. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kwys200801016 [56] 解习农, 叶茂松, 徐长贵, 等, 2018.渤海湾盆地渤中凹陷混积岩优质储层特征及成因机理.地球科学, 43(10):3526-3539. doi: 10.3799/dqkx.2018.277 [57] 杨朝青, 沙庆安, 1990.云南曲靖中泥盆统曲靖组的沉积环境一种陆源碎屑.沉积学报, 8(2): 59-66. [58] 叶蕾, 朱筱敏, 张锐锋, 等, 2020.冀中坳陷饶阳凹陷蠡县斜坡古近系沙河街组一段浅水三角洲和滩坝的沉积环境.古地理学报, 22(3):587-600. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gdlxb202003015 [59] 殷杰, 王权, 郝芳, 等, 2017.渤海湾盆地饶阳凹陷沙一下亚段古湖泊环境与烃源岩发育模式.地球科学, 42(7): 1209-1222. doi: 10.3799/dqkx.2017.098 [60] 张雄华, 2000.混积岩的分类和成因.地质科技情报, 19(4):32-34. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzkjqb200004006 [61] 赵贤正, 卢学军, 崔周旗, 等, 2012.断陷盆地斜坡带精细层序地层研究与勘探成效.地学前缘, 19(1): 10-19. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy201201003 [62] 赵增义, 赵建华, 王海静, 等, 2007.准噶尔盆地微量元素的分布特征及其应用.天然气勘探与开发, 30(2): 30-32, 40. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=trqktykf200702007 [63] 朱筱敏, 谈明轩, 董艳蕾, 等, 2019.当今沉积学研究热点讨论:第20届国际沉积学大会评述.沉积学报, 37(1): 1-16. [64] 朱筱敏, 信荃麟, 张晋仁, 等, 1994.断陷湖盆滩坝储集体沉积特征及沉积模式.沉积学报, 12(2): 20-28. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199400005184 -
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