Sedimentary Features and Development Pattern of Mixed Deposition of Paleogene System in Bohai Sea Area
-
摘要: 陆源碎屑与湖相碳酸盐混合沉积在渤海海域古近系普遍发育，已经成为重要的油气勘探目标.基于90余口已钻井，结合地震、测井以及相关分析化验资料，以渤海海域古近系钻遇的混合沉积为研究对象，开展了沉积特征与成因背景分析，建立了混合沉积发育模式.研究表明：渤海古近系混合沉积发育近岸混积扇、近岸混积滩坝、远岸混积滩坝3种沉积相、7种沉积亚相和14种沉积微相.近岸混积扇以发育混积沟道为典型特征，岩性为含生屑的砂砾岩或中粗砂岩，为陡坡扇三角洲环境短源水道废弃后与生物碎屑间歇性间互沉积；近岸混积滩坝，为近源搬运沉积的陆源碎屑与盆内碎屑之间的混合沉积，典型沉积特征为发育高陆源碎屑含量的各种粒屑滩或坝；远岸混积滩坝为典型的以富含生物碎屑为主的混合沉积，陆源碎屑含量低，一般为盆内低隆或孤立潜山之上原地生长生物与少量供给的陆源碎屑发生的混合沉积.混合沉积发育模式和规模受古气候与古水体环境、古构造与水动力、陆源碎屑物质供给、古地貌条件等共同控制，其中古地貌特征起主导作用.混合沉积发育模式的建立，对混积型储层预测和油气勘探具有重要意义.Abstract: The mixed deposition of terrigenous siliciclastic and lacustrine carbonates is pervasively developed in Paleogene system of Bohai Sea area. Based on drilling, sesimic, well logging and lithological testing data of 90 wells in the mixed deposition of Paleogene system of Bohai Sea area, sedimentary features and forming background were analyzed and the mixed deposition development model was established. Our research indicates that three types of sedimentary facies, including mixed fan, nearshore mixed bar, and offshore mixed bar, which could be further divided into seven types of sub facies and fourteen types of micro facies, are developed in Paleogene strata of the interest area. Nearshore mixed fan, which is normally associated with delta facies and formed near the intrabasinal local provenance of the steep slope zone, is featured with mixed deposited gully with bioclastic sandy conglomerate, and medium-coarse and medium sandstones is featured with the sedimentary facies of which is abandoned fan delta short axial source channel and bioclastic interval deposition. Nearshore mixed bar, which is generally formed near the intrabasinal local provenance of the lake bay, is featured with the mixed deposition of near source transportation sediments and intrabasinal clastic sediments. The typical sedimentary nearshore mixed bar is featured with grained clast bars of high terrigenous clastic content. Offshore mixed bar, which is developed on low uplift or isolated buried hill, is featured with rich bioclastic mixed deposits, low terrigenous clastic content, in-situ development of biology and low supply of terrigenous siliciclastics mixing. The pattern and scale of the mixed deposition are controlled by the interation of paleoclimate environment, paleotectonic activity, hydrodynamic condition, terrigenous siliciclastic supply, with the ancient landform as the most dominant factor. The establishment of the mixed depositional model could play a significant role in the future reservoir prediction and oil exploration.
-
图 1 渤海海域构造单元划分与主要混合沉积分布
Fig. 1. Tectonic units and distribution of mixed sedimentation of Bohai Sea area
图 2 渤海海域古近系综合柱状图
Fig. 2. Comprehensive diagram indicating Paleogene system of Bohai Sea area
图 3 近岸混积扇典型特征：Q29-5井为例
Fig. 3. Typical features of nearshore mixed fan: taking well Q29-5 for example
图 4 近岸（湖湾型）混积滩坝典型特征：Q36-2井为例
Fig. 4. Typical features of (lake bay) nearshore mixed bar: taking well Q36-2 for example
图 5 近岸（低隆型）混积滩坝典型特征：B36-W井为例
Fig. 5. Typical features of (low uplift) offshore mixed bar: taking well B36-W for example
图 6 （硬底型）远岸混积滩坝典型特征：J20构造为例
Fig. 6. Typical features of (sandy) offshore mixed bar: taking structure J20 for example
图 7 （软底型）远岸混积滩坝典型发育特征：以Q30构造为例
Fig. 7. Typical features of (muddy) offshore mixed bar: taking structure Q30 for example
图 8 渤海海域秦皇岛地区沙一二段微量元素及气候、水体环境分析
Fig. 8. Trace element, climate condition and water environment in Paleogene strata of Qinhuangdao region of Bohai Sea area
图 9 渤海海域混积岩发育与古地貌特征耦合关系直方图
Fig. 9. Diagram reflecting the coupling relationship of mixed sediments development with paleogeomorphic feature in Paleogene strata of Bohai Sea area
图 10 渤海海域古近系混合沉积发育综合模式
Fig. 10. Comprehensive model of Paleogene mixed sediments of Bohai Sea area
表 1 渤海海域古近系混合沉积相划分
Table 1. Sedimentary facies division of the mixed deposits in Paleogene system of Bohai Sea area
沉积相 亚相 微相 典型岩石类型 主要发育层段 典型构造及取心井 近岸混积扇 近岸混积扇根 近端沟道 正常沟道沉积的砾岩 沙一二段 Q29-4井 近岸混积扇中 混积沟道 含生屑砂砾岩 Q29-4井、Q29-5井 混积碎屑滩 含生屑中-粗粒砂岩 Q29-4井、Q29-5井 混积生屑（粒屑）滩 含陆屑生屑白云岩 Q29-4井、Q29-5井 近岸混积扇缘 （含生屑）灰质或云质细-粉砂岩 B27-2井 近岸混积滩坝 近岸混积坝 砾质混积坝 含生屑砾岩 沙一二段为主，沙三段 L25-2井 砂质混积坝 含生屑砂岩 L25-2井 近岸混积滩 混积泥质滩 灰质泥岩 B36-W井 混积泥晶滩 泥晶灰岩/云岩 B36-W井 混积生屑（粒屑）滩 含陆屑生屑白云岩 Q36-2井、S36-15井 混积碎屑滩 含生屑中-粗砂岩 Q36-2井、B36-W井 远岸混积滩坝 远岸混积坝 砾质混积坝 含生屑砾岩 沙一二段沙四段 C2-2井、J20-1井、J20-2井 远岸混积滩 混积生屑（粒屑）滩 （含陆屑）生屑白云岩 C2-2井、J20-2井、J20-5、J20-6、B13-2井 混积碎屑滩 含内碎屑中-粗砂岩 B13-3井 混积泥晶滩 泥晶灰岩/白云岩 J20-4井、J20-5井、J20-6井 
下载: 导出CSV
-
[1] Bruckner, W.D., 1953. Cyclic Calcareous Sedimentation as an Index of Climatic Variations in the Past. SEPM Journal of Sedimentary Research, 23(4): 235-237. https://doi.org/10.1306/d4269620-2b26-11d7-8648000102c1865d [2] Cai, J.G., Li, C.X., 1994. Characteristics of Carboniferous Mixed Siliciclastic and Carbonate Sediments in Southwest Inner Mongolia. Oil & Gas Geology, 15(1):80-86(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYYT401.007.htm [3] Coffey, B.P., Read, J.F., 2004. Mixed Carbonate-Siliciclastic Sequence Stratigraphy of a Paleogene Transition Zone Continental Shelf, Southeastern USA. Sedimentary Geology, 166(1-2): 21-57. https://doi.org/10.1016/j.sedgeo.2003.11.018 [4] Davis, R.A.Jr., Cuffe, C.K., Kowalski, K.A., et al., 2003. Stratigraphic Models for Microtidal Tidal Deltas; Examples from the Florida Gulf Coast. Marine Geology, 200(1-4): 49-60. https://doi.org/10.1016/s0025-3227(03)00164-6 doi: 10.1016/S0025-3227(03)00164-6 [5] 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 Formationin Huimin Sag:Taking Shanghe Area in Shandong Province for an Example. Acta Sedimentologica Sinica, 25(3):343-350(in Chinese with English abstract). [6] 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://en.cnki.com.cn/Article_en/CJFDTotal-SYYT201101014.htm [7] Du, X.F., Pang, X.J., Wang, Q.B., et al., 2017. Restoration of the Paleo-Provenance of the Es12 in the Eastern of Shijiutuo Uplift and Its Control on Reservoir. Earth Science, 42(11): 1897-1909(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201711004 [8] Feng, C., Wang, Q.B., Dai, L.M., et al., 2017. Geochemical Characteristics and Geological Significance of the E3s1 Lacustrine Mixed Sedimentary Rocks in the East Actic Region of Shijiutuo Symon Fault in Qinnan Sag. Journal of Northeast Petroleum University, 41(2): 44-53(in Chinese with English abstract). [9] Feng, J.L., Hu, K., Cao, J., et al., 2011. A Review on Mixed Rocks of Terrigenous Clastics and Carbonates and Their Petroleum-Gas Geological Significance. Geological Journal of China Universities, 17(2): 297-307(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gxdzxb201102015 [10] Gu, J.Y., Ma, F., Ji, L.D., 2009. Types, Characteristics and Main Controlling Factors of Carbonate Platform. Journal of Palaeogeography, 11(1): 21-27(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gdlxb200901003 [11] Jiang, M.S., Sha, Q.A., 1996. Mixed Siliciclastic-Carbonate Sediments during the Lower-Middle Cambrian in the North China Platform. Acta Sedimentologica Sinica, 14(A00): 63-74(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CJXB6S1.008.htm [12] Lai, W.C., Song, Z.Q., Zhou, X.H., et al., 2010. Model of Dynamic Source Controlling Sand. Petroleum Exploration and Development, 37(6):763-768(in Chinese with English abstract). http://www.zhangqiaokeyan.com/academic-journal-cn_petroleum-exploration-development_thesis/0201218160011.html [13] 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 [14] Ma, Y.P., Liu, L., 2003. Sedimentary and Diagenetic Characteristics of Paleogene Lacustrine "Hunji" Rock in Beach District, Dagang. Acta Sedimentologica Sinica, 21(4): 607-613 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cjxb200304011 [15] Meng, Z.H., Feng, B., Wang, G.M., 2009. Sedimentation of Mixed Bioclastic Shallows of Steep Slope Zone in Gubei Depression. Petroleum Geology and Engineering, 23(6): 9-11(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hnsy200906003 [16] 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)12<432:MOSACS>2.0.CO;2 [17] Mount, J.F., 1985. Mixed Siliciclastic and Carbonate Sediments: A Proposed First‐Order Textural and Compositional Classification. Sedimentology, 32(3): 435-442. https://doi.org/10.1111/j.1365-3091.1985.tb00522.x [18] 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). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GDLX201705008.htm [19] 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 [20] Song, Z.Q., Du, X.F., Wang, Q.M., et al., 2017. Source-to-Sink System Fine Description and Petroleum Exploration Practice of the Northern Section of Liaoxi Low Uplift. Earth Science, 42(11): 2069-2080(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201711016 [21] Tcherepanov, E.N., Droxler, A.W., Lapointe, P., et al., 2008. Neogene Evolution of the Mixed Carbonate-Siliciclastic System in the Gulf of Papua, Papua New Guinea. Journal of Geophysical Research Atmospheres, 113(F1): F01S21. https://doi.org/10.1029/2006jf000684 http://www.onacademic.com/detail/journal_1000035773272810_22a5.html [22] Wang, B.Q., Hu, M.Y., Hu, A.M., et al., 1993. Mixed Carbonate-Terrigenous Clastic Sediments of Middle Triassic Badong Formation in Nanzhang, Hubei. Oil & Gas Geology, 14(4): 285-290(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYYT199304003.htm [23] Wang, Q.B., Liu, L., Niu, C.M., et al., 2019. The Geological Evidences and Impacts of Deep Thermal Fluid on Lacustrine Carbonate Reservoir in the Actic Area of the North Part of Bozhong Depression, Bohai Bay Basin. Earth Science, 44(8):2751-2760(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201908019 [24] Xi, 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 [25] 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). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CJXB199002008.htm [26] Ye, M.S., Xie, X.N., Xu, C.G., et al., 2018. Discussion for Classification-Designation System of Mixed Siliciclastic-Carbonate Sediments and the Implication for Their Reservoir Prediction: A Case Study of Mixed Sediments from Bohai Sea Area. Geological Review, 64(5):1118-1131(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DZLP201805007.htm [27] Zhang, D., Hou, Z.J., Wang, Y.H., et al., 2008. Sedimentary Characteristics of Lacustrine Carbonate Rocks of the First Member of Shahejie Formation in Banqiao-Beidagang Area. Northwest Oil & Gas Exploration, 20(4): 92-97, 131(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yxyqc200804017 [28] Zhang, L., Wang, D.Y., Zhang, X.T., et al., 2019. The Controlling Factors of the High-Quality Mixed Reservoirs in QHD29-2E Structure, Bohai Sea. Acta Sedimentologica Sinica, 37(1): 200-211(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cjxb201901019 [29] 蔡进功, 李从先, 1994.内蒙西南部石炭系碎屑岩_碳酸盐岩混合沉积特征.石油与天然气地质, 15(1):80-86. http://www.cnki.com.cn/Article/CJFDTotal-SYYT401.007.htm [30] 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. http://www.cqvip.com/Main/Detail.aspx?id=24912038 [31] 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 [32] 杜晓峰, 庞小军, 王清斌, 等, 2017.石臼坨凸起东段围区沙一二段古物源恢复及其对储层的控制.地球科学, 42(11): 1897-1909. doi: 10.3799/dqkx.2017.120 [33] 冯冲, 王清斌, 代黎明, 等, 2017.秦南凹陷石东陡坡带沙一段陆相混积岩地球化学特征及其地质意义.东北石油大学学报, 41(2): 44-53. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqsyxyxb201702005 [34] 冯进来, 胡凯, 曹剑, 等, 2011.陆源碎屑与碳酸盐混积岩及其油气地质意义.高校地质学报, 17(2): 297-307. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gxdzxb201102015 [35] 顾家裕, 马锋, 季丽丹, 2009.碳酸盐岩台地类型、特征及主控因素.古地理学报, 11(1): 21-27. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gdlxb200901003 [36] 江茂生, 沙庆安, 1996.华北地台下中寒武统碳酸盐与陆源碎屑混合沉积——以山东张夏地区为例.沉积学报, 14(A00): 63-74. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199600895927 [37] 赖维成, 宋章强, 周心怀, 等, 2010. "动态物源"控砂模式.石油勘探与开发, 37(6): 763-768. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=syktykf201006018 [38] 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 [39] 马艳萍, 刘立, 2003.大港滩海区第三系湖相混积岩的成因与成岩作用特征.沉积学报, 21(4):607-613. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cjxb200304011 [40] 孟兆鸿, 冯斌, 王冠民, 2009.孤北洼陷陡坡带的混合生屑浅滩沉积.石油地质与工程, 23(6): 9-11. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hnsy200906003 [41] 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屑白云岩成因.古地理学报, 19(5): 835-848. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gdlxb201705006 [42] 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 [43] 宋章强, 杜晓峰, 王启明, 等, 2017.辽西低凸起北段源-汇系统精细描述与油气勘探实践.地球科学, 42(11): 2069-2080. doi: 10.3799/dqkx.2017.132 [44] 王宝清, 胡明毅, 胡爱梅, 等, 1993.湖北南漳中三叠统巴东组碳酸盐与陆源碎屑混合沉积.石油与天然气地质, 14(4): 285-290. http://www.cqvip.com/Main/Detail.aspx?id=1162776 [45] 王清斌, 刘立, 牛成民, 等, 2019.渤中凹陷北部陡坡带热液活动及其对湖相碳酸盐岩储层的影响.地球科学, 44(8):2751-2760. doi: 10.3799/dqkx.2018.347 [46] 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 [47] 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. http://www.cqvip.com/QK/95994X/19902/221837.html [48] 叶茂松, 解习农, 徐长贵, 等, 2018.混积岩分类命名体系探讨及对混积岩储层评价的启示——以渤海海域混积岩研究为例.地质评论, 64(5):1118-1131. http://www.cnki.com.cn/Article/CJFDTotal-DZLP201805007.htm [49] 张娣, 侯中健, 王亚辉, 等, 2008.板桥-北大港地区沙河街组沙一段湖相碳酸盐岩沉积特征.岩性油气藏, 20(4): 92-97, 131. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yxyqc200804017 [50] 张藜, 王德英, 张新涛, 等, 2019.渤海海域秦皇岛29-2东构造优质混积储层主控因素.沉积学报, 37(1): 200-211. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cjxb201901019 -
点击查看大图
图(10) / 表(1)
计量
- 文章访问数: 520
- HTML全文浏览量: 291
- PDF下载量: 52
- 被引次数: 0
