Paleobiological Characteristics and Its Reservoir Significance of Bioclastic Migmatite in First Member of Shahejie Formation in Bohai Sea
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摘要: 渤海海域古近系沙一段广泛发育湖相混积岩，其中生物碎屑混积岩物性好、产能高，是混积岩中的优质储层.对生物碎屑混积岩中的生物碎屑成分展开系统的古生物研究，明确腹足类是渤海海域沙一段生物碎屑混积岩中最主要的生物碎屑类型，共鉴定出腹足类21属27种，介形类19属74种，并且均以适宜一定盐度浅水环境生活的小型化类型为主.结合古环境研究表明，高能环境腹足类易富集，相对低能环境介形类含量上升.通过铸体薄片、扫描电镜、电子探针等分析发现，生物碎屑对混积岩储层演化具有重要影响.生物碎屑体腔孔、壳体铸模孔、遮蔽孔、差异收缩缝直接提供了储集空间；生物碎屑早期溶蚀能有效改善储层渗透能力，促进生物碎屑富集段的白云岩化作用，形成生物碎屑白云岩优质储层；生物碎屑在微生物作用下形成性质稳定的泥晶套，起到了孔隙格架支撑作用.受壳体成分及各门类生物沉积环境差异影响，腹足类为主的生物碎屑混积岩物性更好.Abstract: Lacustrine migmatite is widely distributed in the first member of Shahejie Formation of Paleogene in Bohai Sea. The bioclastic migmatite is the high-quality reservoir with good physical properties and high productivity. In this paper, a systematic paleontological study of bioclastic components in bioclastic migmatites is carried out. It is confirmed that gastropods are the most important bioclastic types in the first member of the Shahejie Formation in Bohai Sea. 21 genus and 27 species of gastropods and 19 genus and 74 species of ostracoda are identified. They are mainly miniaturized types suitable for living in a certain salinity and shallow water environment. It is found that the gastropods are easily to accumulate in high energy environment, while the content of ostracods is relatively high in low energy environment combined with paleoenvironmental studies. The analyses of casting thin section, SEM and EPMA show that bioclasts play an important role in the evolution of migmatite reservoir. The reservoir space is directly provided by the cavity hole of the bioclastic body, the mold hole of the shell, the shielding hole and the differential contraction joint. Early dissolution of bioclasts can effectively improve the permeability of the reservoir, promote dolomitization of the bioclastic enrichment section, and form a high-quality reservoir of bioclastic dolomite. Bioclasts form a stable mud crystal set with the action of microorganism, which plays a supporting role of pore lattice. The physical properties of the bioclastic migmatite mainly composed of gastropods are better than the others, as influenced by the differences of shell composition and various kinds of biological sedimentary environment.
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Key words:
- Bohai Sea area /
- Paleogene /
- bioclastic migmatite /
- palaeontology /
- reservoir /
- sedimentation
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图 1 渤海海域构造位置及沙河街组岩性综合柱状图
Fig. 1. Structural location of the Bohai Sea area and the generalized stratigraphy of the Shehejie Formation
图 2 渤海海域古近系湖相生物碎屑混积岩中常见化石照片
a. BZ262A井, 3 264.51 m，小恒河螺Gangetia minys；b. BZ262A井，3 250.20 m，小恒河螺Gangetia minys；c. BZ262A井, 3 264.51 m，细弱恒河螺Gangetia exilis；d. BZ262A井, 3 264.51 m，短圆恒河螺Gangetia brevirota；e. BZ262A井, 3 264.51 m，均匀狭口螺Stenothyra paritis；f. BZ262A井, 3 264.51 m，优美狭口螺Stenothyra elegans；g. BZ262A井, 3 264.51 m，狭口螺属未定种Stenothyra sp.；h. BZ262A井，3 250.20 m，热河台高盘螺Valvata rehetaiensis；i. BZ262A井, 3 264.51 m，下辽副贝加尔螺？Parabaicalia xialiaoensis？；j. BZ262A井，3 264.51 m，乐陵真星介Eucypris lelingensis；k. BZ262A井，3 264.51 m，玻璃介未定种Candona sp.. 图 2a~2h线段比例尺=1 mm
Fig. 2. Photos of fossils in the lacustrine bioclastic migmatite of Paleogene, Bohai Sea area
图 3 渤海海域沙一段生物碎屑混积岩中化石频率统计
Fig. 3. Drilling frequency statistics of fossils in bioclastic migmatite in the first member of Shahejie Formation in Bohai Sea area
图 4 不同沉积环境生物碎屑特征
a.QHD292E井，陡坡带古地貌背景；b.BZ262A井，平缓古地貌背景；c.QHD292E井，3 343.55 m生物碎屑混积岩中腹足类化石；d.BZ262A井，3 250.68 m生物碎屑混积岩中介形虫碎片
Fig. 4. Characteristics of bioclastics in different sedimentary environments
图 5 生物碎屑混积岩孔渗分布特征
a.生物碎屑混积岩物性特征；b.不同生物碎屑类型孔渗分布对比
Fig. 5. The porosity and permeability distribution of bioclastic migmatite
图 6 生物碎屑对湖相混积岩储层的改善作用
a. QHD292EB井，3 353.50 m，生物体腔孔；b. B362Q井，2 390.25 m，介形虫体腔孔发育，部分被粉晶白云石胶结充填；c. QHD292ED井，3 433.00 m，生物碎屑遮蔽孔发育；d. QHD292E井，3 370.36 m，生物碎屑遮蔽孔发育；e. QHD292E井，3 382.14 m，遮蔽孔；f. BZ262A井，3 257.10 m，铸模孔大量发育，仅剩泥晶套；g. BZ262A井, 3 252.06 m, 生物碎屑铸模孔；h. BZ262A井，3 263.96 m，铸模孔发育，部分生物碎屑体腔被充填；i. B362Q井，2 381.60 m，微裂缝沿介形壳体裂开、扩散
Fig. 6. Improvement of lacustrine migmatite reservoir by bioclastic
图 8 B362Q生物碎屑混积岩井段综合柱状图
Fig. 8. The generalized stratigraphy of bioclastic migmatite of well B362Q
图 9 泥晶套扫描电镜特征
a.B362Q井，2 394.20 m，生物碎屑泥晶套背闪射照片；b. B362Q井，2 394.20 m，生物碎屑泥晶套局部背闪射特征（同图a中红色标注视域）
Fig. 9. Characteristics of micrite envelope
表 1 QHD292E井与BZ262A井元素分析
Table 1. Analysis data of typical elements of Well QHD292E and Well BZ262A
井号 深度(m) Ni(g/g) Co(g/g) MnO(%) Fe2O3(%) Ni/Co MnO/Fe2O3 Ni/Co平均值 MnO/Fe2O3平均值 QHD292E 3 255 46.70 19.40 0.08 3.70 2.41 0.02 2.15 0.03 QHD292E 3 320 25.60 12.70 0.07 1.82 2.02 0.04 QHD292E 3 335 23.30 12.60 0.06 1.69 1.85 0.04 QHD292E 3 390 15.50 7.43 0.06 1.19 2.09 0.05 QHD292E 3 430 9.75 4.36 0.03 1.24 2.24 0.02 QHD292E 3 475 14.50 6.26 0.11 2.78 2.32 0.04 BZ262A 3 195 36.93 15.68 0.30 2.49 2.36 0.12 2.51 0.14 BZ262A 3 215 34.48 13.34 0.33 2.26 2.59 0.15 BZ262A 3 225 33.68 13.98 0.31 2.17 2.41 0.14 BZ262A 3 235 33.68 14.31 0.32 2.16 2.35 0.15 BZ262A 3 246 20.97 8.99 0.67 4.19 2.33 0.16 BZ262A 3 278 44.60 16.72 0.42 4.57 2.67 0.09 BZ262A 3 290 32.31 14.45 0.34 3.28 2.24 0.10 BZ262A 3 300 50.72 17.12 0.42 2.95 2.96 0.14 BZ262A 3 310 38.85 15.54 0.42 2.87 2.50 0.15 BZ262A 3 320 33.39 12.45 0.38 2.45 2.68 0.15 
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表 2 B362Q井生物碎屑混积岩井段碳、氧同位素值
Table 2. Analysis data of carbon and oxygen isotopes in bioclastic migmatite of Well B362Q
样号 深度(m) 层位 岩石类型 δ13C(‰，PDB) δ18O(‰，PDB) 古盐度S(‰) 古盐度指数Z 古温度(℃) B362Q 2 386.42 沙一段 生物碎屑 2.60 -7.22 27.53 129.03 48.71 B362Q 2 386.95 沙一段 鲕粒 1.97 -9.40 25.35 126.65 60.06 B362Q 2 391.00 沙一段 生物碎屑 0.15 -14.85 19.90 120.21 90.09 B362Q 2 392.45 沙一段 泥晶套 1.75 -11.30 23.45 125.26 70.26 B362Q 2 394.20 沙一段 砂屑 2.55 -5.57 29.18 129.75 40.38 B362Q 2 395.00 沙一段 砂屑 2.76 -6.00 28.75 129.96 42.53 B362Q 2 395.00 沙一段 洞充填物 1.49 -6.70 28.05 127.01 46.06 B362Q 2 395.70 沙一段 泥晶云岩 -0.50 -6.53 28.22 123.02 45.20 B362Q 2 396.10 沙一段 泥晶云岩 0.04 -2.62 32.13 126.08 26.02 B362Q 2 396.10 沙一段 泥晶云岩 0.40 -3.70 31.05 126.28 31.20 B362Q 2 396.50 沙一段 泥晶云岩 0.74 -2.19 32.56 127.72 23.98 注：古盐度S=δ18OPDB +21.2/0.61；古盐度指数Z=2.048×（δ13CPDB+50）+0.498×（δ18OPDB+50）；古温度T=13.85-4.54×δ18OPDB +0.04×(δ18OPDB)2.据Keith and Weber(1964).
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表 3 生物碎屑壳体电子探针数值
Table 3. EPMA data of bioclastic shell
井号 井深（m） 点号 MgO(%) QHD292E 3 375.65 1 45.05 QHD292E 3 375.65 2 40.18 QHD292E 3 375.65 3 41.49 QHD292E 3 375.65 4 39.41
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[1] Bi, Y.Q., Tian, H.Q., Zhao, Y.S., et al., 2001. On the Micrite Envelope to Restoration of Primary Texture Character of Secondary Dolomites and Its Significance. Acta Petrologica Sinica, 17(3):491-496 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200103019 [2] Ding, Y., Li, Z.W., Feng, F., et al., 2013. Mixing of Lacustrine Siliciclastic:Carbonate Sediments and Its Significance for Tight Oil Exploration in the Daanzhai Member, Ziliujing Formation, Lower Jurassic, in Longgang Area, Central Sichuan Basin. Geological Review, 59(2):389-400(in Chinese with English abstract). [3] Fu, X.D., Wu, J.P., Shou, J.F., et al., 2019. Tight Oil Reservoir Characteristics of Lacustrine Mixed Marlstone in the Palaeogene Shahejie Formation of Shulu Sag, Bohai Bay Basin. Oil & Gas Geology, 40(1):78-91(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=syytrqdz201901008 [4] Hagadorn, J.W., Bottjer, D.J., 1997. Wrinkle Structures:Microbially Mediated Sedimentary Structures Common in Subtidal Siliciclastic Settings at the Proterozoic-Phanerozoic Transition. Geology, 25(11):1047. https://doi.org/10.1130/0091-7613(1997)0251047:wsmmss>2.3.co; 2 doi: 10.1130/0091-7613(1997)025<1047:WSMMSS>2.3.CO;2 [5] Huang, L., Zhou, X.H., Liu, C.Y., et al., 2012. The Important Turning Points during Evolution of Cenozoic Basin Offshore the Bohai Sea:Evidence and Regional Dynamics Analysis. Science China Earth Sciences, 42(6):893-904 (in Chinese). [6] Huo, S.J., Yang, X.H., Wang, Q.B., et al., 2015. Controlling Factors on Diamictite Reservoir in Shahejie Formation, H-1 Structure, Huanghekou Depression. Geoscience, 29(6):1348-1359(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xddz201506009 [7] 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. https://doi.org/10.1016/0016-7037(64)90022-5 [8] Li, J.Z., Yan, K., Ren, H.Q., et al., 2020. Detailed Quantitative Description of Fluvial Reservoirs:A Case Study of L6-3 Layer of Sandgroup 6 in the Second Member of Shahejie Formation, Shengtuo Oilfifield, China. Advances in Geo-Energy Research, 4(1):43-53, https://doi.org/10.26804/ager.2020.01.05. [9] Lü, Z.X., Wang, X.D., Wu, J.Y., et al., 2018. Diagenetic Evolution Characteristics of Paleogene Lacustrine Carbonate Reservoirs in the Central Bohai Sea Area. Natural Gas Geoscience, 29(7):921-931(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=trqdqkx201807001 [10] Ni, J.E., Sun, L.C., Gu, L., et al., 2013. Depositional Patterns of the 2nd Member of the Shahejie Formation in Q Oilfield of the Shijiutuo Uplift, Bohai Sea. Oil & Gas Geology, 34(4):491-498(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=syytrqdz201304010 [11] Pan, W.J., Wang, Q.B., Liu, S.L., et al., 2017. Origin of Lacustrine Bioclastic Dolostone in the Paleogene Shahejie Formation:A Case Study in Shijiutuo Area, Bohai Sea. Journal of Palaeogeography, 19(5):835-848(in Chinese with English abstract). [12] Pang, S.Y., Cao, Y.C., Liang, C., 2019. Lithofacies Characteristics and Sedimentary Environment of Es4U and Es3L:A Case Study of Well FY1 in Dongying Sag, Bohai Bay Basin. Oil & Gas Geology, 40(4):799-809(in Chinese with English abstract). [13] 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). [14] 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 [15] Yan, J.H., Deng, Y., Pu, X.G., et al., 2017. Characteristics and Controlling Factors of Fine-Grained Mixed Sedimentary Rocks from the 2nd Member of Kongdian Formation in the Cangdong Sag, Bohai Bay Basin. Oil & Gas Geology, 38(1):98-109(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=syytrqdz201701012 [16] Yang, Z.Y., Luo, P., Liu, B., et al., 2017.The Difference and Sedimentation of Two Black Rock Series from Yurtus Formation during the Earliest Cambrian in the Aksu Area of Tarim Basin, Northwest China. Acta Petrologica Sinica, 33(6):1893-1918 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201706017 [17] Zhang, D.N., Yang, Y., Hu, J.F., et al., 2019. Occurrence of Aliphatic Biopolymer in Chlorophyceae Algae and Cyanobacteria-Rich Phytoplankton. Organic Geochemistry, 135:1-10. https://doi.org/10.1016/j.orggeochem.2019.04.008 [18] Zhang, J., Zhang, B.S., Shan, X.Q., 2014.Controlling Effects of Paleo-Climate and Paleo-Ocean on Formation of Carbonate Reservoirs.Petroleum Exploration and Development, 41(1):121-128(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=syktykf201401016 [19] Zhang, N.S., Ren, X.J., Wei, J.X., et al., 2006. Rock Types of Mixosedimentite Reservoirs and Oil-Gas Distribution in Nanyishan of Qaidam Basin. Acta Petrolei Sinica, 27(1):42-46(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=syxb200601009 [20] Zhao, W.Z., Shen, A.J., Hu, A.P., et al., 2015. A Discussion on the Geological Background of Marine Carbonate Reservoirs Development in Tarim, Sichuan and Ordos Basin, China. Acta Petrologica Sinica, 31(11):3495-3508(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201511024 [21] 毕义泉, 田海芹, 赵勇生, 等, 2001.论泥晶套与次生白云岩原岩结构特征的恢复及意义.岩石学报, 17(3):491-496. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200103019 [22] 丁一, 李智武, 冯逢, 等, 2013.川中龙岗地区下侏罗统自流井组大安寨段湖相混合沉积及其致密油勘探意义.地质论评, 59(2):389-400. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzlp201302020 [23] 付小东, 吴健平, 寿建峰, 等, 2019.渤海湾盆地束鹿凹陷古近系沙河街组湖相混积泥灰岩致密油储层特征.石油与天然气地质, 40(1):78-91. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=syytrqdz201901008 [24] 黄雷, 周心怀, 刘池洋, 等, 2012.渤海海域新生代盆地演化的重要转折期——证据及区域动力学分析.中国科学:地球科学, 42(6):893-904. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgkx-cd201206008 [25] 霍沈君, 杨香华, 王清斌, 等, 2015.黄河口凹陷H-1构造沙河街组混积岩储层控制因素.现代地质, 29(6):1348-1359. [26] 吕正祥, 王先东, 吴家洋, 等, 2018.渤海海域中部古近系湖相碳酸盐岩储层成岩演化特征.天然气地球科学, 29(7):921-931. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=trqdqkx201807001 [27] 倪军娥, 孙立春, 古莉, 等, 2013.渤海海域石臼坨凸起Q油田沙二段储层沉积模式.石油与天然气地质, 34(4):491-498. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=syytrqdz201304010 [28] 潘文静, 王清斌, 刘士磊, 等, 2017.渤海海域石臼坨地区古近系沙河街组湖相生物碎屑白云岩成因.古地理学报, 19(5):835-848. [29] 逄淑伊, 操应长, 梁超, 2019.渤海湾盆地东营凹陷沙四上亚段-沙三下亚段岩相特征及沉积环境:以樊页1井为例.石油与天然气地质, 40(4):799-809. [30] 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, (S2):234-242. doi: 10.3799/dqkx.2018.138 [31] 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 [32] 鄢继华, 邓远, 蒲秀刚, 等, 2017.渤海湾盆地沧东凹陷孔二段细粒混合沉积岩特征及控制因素.石油与天然气地质, 38(1):98-109. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=syytrqdz201701012 [33] 杨宗玉, 罗平, 刘波, 等, 2017.塔里木盆地阿克苏地区下寒武统玉尔吐斯组两套黑色岩系的差异及成因.岩石学报, 33(6):1893-1918. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201706017 [34] 张静, 张宝民, 单秀琴, 2014.古气候与古海洋对碳酸盐岩储集层发育的控制.石油勘探与开发, 41(1):121-128. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=syktykf201401016 [35] 张宁生, 任晓娟, 魏金星, 等, 2006.柴达木盆地南翼山混积岩储层岩石类型及其与油气分布的关系.石油学报, 27(1):42-46. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=syxb200601009 [36] 赵文智, 沈安江, 胡安平, 等, 2015. 塔里木、四川和鄂尔多斯盆地海相碳酸盐岩规模储层发育地质背景初探. 岩石学报, 31(11):3495-3508. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201511024 -
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