Geophysical Integrated Prediction Technology of Mixed Rock Reservoir with Genetic Environment Constraints in Bohai Sea Area
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摘要: 勘探实践表明,混合沉积逐渐成为渤海海域中深部勘探的理想领域.通过大量钻井资料统计,揭示了渤海海域混合沉积的成因条件,认为渤海海域混积岩的形成受气候与水体环境、物源、古地貌条件以及沉积样式的控制.模型正演表明不同厚度以及不同地层岩性组合的混积岩地震响应特征不同.实例表明,在水体气候环境、物源类型、古地貌特征等成因环境约束的条件下,通过单井分析、地震相分析、微古地貌恢复、正演分析、属性分析、叠前反演等多种技术综合的以“成因模式找规律,地震技术描分布”的混积型储层综合预测技术组合在渤海海域混合沉积储层预测中是可行的,其中不同厚度及岩性组合混积型储层采取不同的储层预测关键技术对渤海海域混积岩勘探有较好的指导意义.Abstract: Mixed sediment has gradually become an ideal area for deep exploration in Bohai Sea area in exploration practice. Through a large number of drilling data statistics,in this paper,it reveals the genetic conditions of mixed sediments in the Bohai Sea area. It is believed that the formation of mixed rock in Bohai Sea area is controlled by climate,water environment,provenance,paleogeomorphic conditions and sedimentary patterns. The forward modeling results show that the seismic response characteristics of the mixed rock with different thickness and different formation lithology combinations are different. Examples show that,under the constraints of the genetic environment,such as climate environment,provenance type and paleogeomorphic characteristics,it is feasible to use the combination of "genetic model to find the rule,seismic technique to trace the distribution" in the prediction of mixed sedimentary reservoirs through the combination of single well analysis,seismic facies analysis,micro-paleogeomorphology recovery,forward modeling analysis,attribute analysis and other technologies. Different key techniques of reservoir prediction for mixed type reservoirs with different thickness and lithologic combination are of significance for the exploration of mixed rock in Bohai Sea area.
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Key words:
- mixed sediment /
- genetic environment /
- reservoir prediction /
- forward analysis /
- Bohai Sea area /
- sedimentation
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图 6 地震正演模型及结果
a.泥岩-混积岩-火山岩正演模型; a’.泥岩-混积岩-火山岩正演结果; b.泥岩-混积岩-砂岩正演模型; b’.泥岩-混积岩-砂岩正演结果; c.泥岩-生物碳酸盐岩混积岩-火山岩正演模型; c’.泥岩-生物碳酸盐岩混积岩-火山岩正演结果d.泥岩-生物碳酸盐岩混积岩-火山岩正演模型; d’.泥岩-生物碳酸盐岩混积岩-火山岩正演结果; e.泥岩-砂岩-火山岩正演模型; e’.泥岩-砂岩-火山岩正演结果; f.泥岩-火山岩正演模型; f’.泥岩-砂岩-火山岩正演结果; g.不同频带地层厚度与振幅关系
Fig. 6. Seismic forward model and results
表 1 不同类型储层地震响应特征及关键地球物理技术
Table 1. Seismic response characteristics and key geophysical techniques of different types of reservoirs
储层类型 地震响应特征 关键地球物理技术 厚储层 较明显的地震构型以及外形特征以及较强振幅 古地貌恢复技术、地震正演技术、地震相分析技术 薄储层 下伏地层岩性为碎屑岩 强振幅连续反射 古地貌恢复技术、地震相分析技术、多属性储层预测技术 下伏地层岩性为火山岩 低频强振幅,但与火山岩形成的强振幅难区分 古地貌恢复技术、岩石物理分析、时频域波形分类技术 -
[1] Bruckner, W.D., 1953. Cyclic Calcareous Sedimentation as an Index of Climatic Variations in the Past. Journal of Sedimentary Petrology, 23(4): 235-237. http://www.researchgate.net/publication/250080849_Cyclic_Calcareous_Sedimentation_as_an_Index_of_Climatic_Variations_in_the_Past [2] Campbell, A.E., 2005. Shelf-Geometry Response to Changes in Relative Sea Level on a Mixed Carbonate-Siliciclastic Shelf in the Guyana Basin. Sedimentary Geology, 175(1-4): 259-275. https://doi.org/10.1016/j.sedgeo.2004.09.003 [3] Deng, Y.H., 1991. A Discussion on the Environment of Formation and the Characteristics of the Carbonate Rock in the Shahejie Group in the Liaodong Bay Basin. Petroleum Exploration and Development, 18(6): 32-39(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SKYK199106005.htm [4] 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). http://www.cnki.com.cn/Article/CJFDTotal-SYYT201101014.htm [5] Du, Y.H., 1990. Eogene Lacustrine Carbonate Rocks and Sedimentary Model in Bohai Bay Region. Oil & Gas Geology, 11(4): 376-392, T001, T002(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYYT199004004.htm [6] Feng, J.L., Cao, J., Hu, K., et al., 2011.Forming Mechanism of Middle-Deep Mixed Rock Reservoir in the Qaidam Basin. Acta Petrologica Sinica, 27(8): 2461-2472(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201108022 [7] Liu, W.C., Zhang, G.K., Yang, H.F., et al., 2018.Characteristics and Development Model of Mixed Deposits of the Paleogene in Southern Laizhou Bay Sag, Bohai Sea. Journal of Palaeogeography, 20(6):1033-1042(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gdlxb201806010 [8] Ma, Y.B., Wu, S.G., Xing, S.W., et al., 2012. Stratigraphic Model and Seismic Characteristics of the Mixed Sedimentation in the Slope Area of North South China Sea. Journal of Jilin University(Earth Science Edition), 42(Suppl.1):88-95(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CCDZ2012S1012.htm [9] 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 [10] Palermo, D., Aigner, T., Geluk, M., et al., 2008. Reservoir Potential of a Lacustrine Mixed Carbonate/Siliciclastic Gas Reservoir: The Lower Triassic Rogenstein in the Netherlands. Journal of Petroleum Geology, 31(1): 61-96. https://doi.org/10.1111/j.1747-5457.2008.00407.x [11] 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 [12] Song, Z.Q., Chen, Y.F., Du, X.F., et al., 2013. Study on Sedimentary Characteristics and Reservoir of Second Member of Shahejie Formation, a Structural Area, Bohai Sea. Offshore Oil, 33(4): 13-18(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hysy201304003 [13] Song, Z.Q., Lai, W.C., Niu, C.M., et al., 2009. An Integrated Seismic-Geological Approach to Predict Lacustrine Carbonate Rock in the Bohai Sea Waters. Oil & Gas Geology, 30(4): 444-449(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=syytrqdz200904009 [14] Su, C.G., 2010. Seismic Identification and Prediction of Lacustrine Carbonate at Es4 in Zhanche Area. Oil Geophysical Prospecting, 45(4): 565-570(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=sydqwlkt201004018 [15] Wang, Q.M., Du, X.F., Jia, D.H., et al., 2015. The 1st and 2nd Members of the Shahejie Formation in No. 428 Uplifted Area, Bohai Sea: Sedimentary Systems and Their Controlling Factors. Sedimentary Geology and Tethyan Geology, 35(4): 12-16(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yxgdl201504002 [16] Xia, Q.L., 2016.Innovation of Geological Theories and Exploration Discoveries in Bohai Oil Fields in the Last Decade. China Offshore Oil and Gas, 28(3):1-9 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-ZHSD201603001.htm [17] 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 [18] 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 [19] Yang, Y.J., Liu, J.D., Tian, J.C., et al., 2011. Mixed Sedimentary Characteristics and Controlling Factors of Upper Ordovician Sangtamu Formation in Tarim Basin. Geological Review, 57(2): 185-192(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzlp201102004 [20] 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 [21] Zhang, X.H., 2000.Classification and Origin of Mixosedimentite.Geological Science and Technology Information, 19(4): 31-34(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzkjqb200004006 [22] Zhao, C., Li, X.B., Huan, J.L., et al., 2013. Mechanism of Mixied Siliciclastic: Carbonate Sediments and Its Controlling Factors. Geological Review, 59(4): 615-626(in Chinese with English abstract). http://www.researchgate.net/publication/306151614_Mechanism_of_mixied_siliciclastic-carbonate_sediments_and_its_controlling_factors_J [23] Zheng, D.S., Cheng, Y., Li, M.L., et al., 2015. Sedimentary Characteristics and Controlling Factors of the Mixed Deposits from the Upper Member of the Middle Jurassic Ma'ao Formation in the Jiyuan Basin, Western Henan. Sedimentary Geology and Tethyan Geology, 35(1): 102-108(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-TTSD201501013.htm [24] Zhu, C., Liu, Z.G., Yang, S. Y., et al., 2018.Lacustrine Carbonate Reservoir Prediction in Yingxi, Qaidam Basin with the Facies-Constrained and Segmented-Frequency-Band Inversion. Oil Geophysical Prospecting, 53(4):832-841(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-SYDQ201804022.htm [25] 邓运华, 1991.试论辽东湾坳陷沙河街组碳酸盐岩形成环境及其特征.石油勘探与开发, 18(6): 32-39. http://www.cnki.com.cn/Article/CJFDTotal-SKYK199106005.htm [26] 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 [27] 杜韫华, 1990.渤海湾地区下第三系湖相碳酸盐岩及沉积模式.石油与天然气地质, 11(4): 376-392, T001, T002. http://www.cnki.com.cn/Article/CJFD1990-SYYT199004004.htm [28] 冯进来, 曹剑, 胡凯, 等, 2011.柴达木盆地中深层混积岩储层形成机制.岩石学报, 27(8): 2461-2472. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201108022 [29] 刘文超, 张国坤, 杨宏飞, 等, 2018.渤海莱州湾凹陷南部古近系混合沉积特征及发育模式.古地理学报, 20(6):1033-1042. http://d.old.wanfangdata.com.cn/Periodical/gdlxb201806010 [30] 马玉波, 吴时国, 邢树文, 等, 2012.南海北部陆坡混合沉积地层模式及地震响应特征.吉林大学学报(地球科学版), 42(增刊1).88-95. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=7267278 [31] 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 [32] 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 [33] 宋章强, 陈延芳, 杜晓峰, 等, 2013.渤海海域A构造区沙二段混合沉积特征及储层研究.海洋石油, 33(4): 13-18. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hysy201304003 [34] 宋章强, 赖维成, 牛成民, 等, 2009.渤海海域湖相碳酸盐岩地震-地质综合预测方法及应用.石油与天然气地质, 30(4): 444-449. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=syytrqdz200904009 [35] 苏朝光, 2010.沾车地区沙四段湖相碳酸盐岩的地震识别与预测.石油地球物理勘探, 45(4): 565-570. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=sydqwlkt201004018 [36] 王启明, 杜晓峰, 加东辉, 等, 2015.渤海海域428凸起地区沙一二段沉积体系及其主控因素.沉积与特提斯地质, 35(4): 12-16. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yxgdl201504002 [37] 夏庆龙, 2016.渤海油田近10年地质认识创新与油气勘探发现.中国海上油气, 28(3):1-9. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zghsyq-gc201603001 [38] 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 [39] 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 [40] 杨永剑, 刘家铎, 田景春, 等, 2011.塔里木盆地上奥陶统桑塔木组混合沉积特征及控制因素.地质论评, 57(2): 185-192. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzlp201102004 [41] 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 [42] 张雄华, 2000.混积岩的分类和成因.地质科技情报, 19(4):31-34. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzkjqb200004006 [43] 赵灿, 李旭兵, 郇金来, 等, 2013.碳酸盐与硅质碎屑的混合沉积机理和控制因素探讨.地质论评, 59(4): 615-626. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzlp201304003 [44] 郑德顺, 程涌, 李明龙, 等, 2015.济源盆地中侏罗统马凹组上段混合沉积特征及其控制因素.沉积与特提斯地质, 35(1): 102-108. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yxgdl201501013 [45] 朱超, 刘占国, 杨少勇, 等, 2018.利用相控分频反演预测英西湖相碳酸盐岩储层.石油地球物理勘探, 45(4):565-570. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=sydqwlkt201804022