Gravity Flow Deposits and Its Genetic Mechanism of Dainan Formation in Huangjue-Majiazui District, Gaoyou Subbasin
-
摘要: 苏北盆地勘探开发重点正逐步由寻找构造类油气藏向寻找隐蔽油气藏转变，重力流沉积形成的岩性砂体对隐蔽油气藏的勘探显得日益重要.以岩心、测-录井、地震反射特征等资料对苏北盆地高邮凹陷西南端黄珏-马家嘴地区戴南组沉积砂体及其成因进行研究，结果表明：该区戴南组一段沉积时期主要发育了近岸水下冲积扇、滑塌-浊积扇沉积；戴南组二段沉积时期主要发育了扇三角洲沉积、滑塌-浊积扇沉积.这些沉积砂体的发育与独特的构造样式、活跃的构造背景、外力活动等因素有着密切的联系；滑塌-浊积扇的发现为进一步的油气勘探提供了依据和思路.Abstract: The main exploration targets of petroleum prospecting in Subei Basin shift gradually from structural reservoirs to subtle reservoirs nowadays. As potential gas and oil-bearing reservoirs, gravity flow sediment prospecting becomes more important for subtle reservoirs exploration. Based on the core observation, well logging, seismic profile characters, gravity flow deposits developed in E2d of Huangjue-Majiazui district in Gaoyou sag and their genies are studied. It is found that nearshore subaqueous alluvial fans and slump-turbidities developed in E2d1 in study area, while fan deltas and slump-turbidities developed in E2d2. The development of sandbodies is considered to be closely coordinated with the special structural pattern, special and active tectonic backgrounds. Discovery of slump-turbidities provides theoretical framework for oil and gas exploration.
-
图 1 黄珏马家嘴地区E2d构造、井位
1.井名井位；2.地名；3.断层；4.工区范围；5.剖面位置
Fig. 1. Structural and well location map in Huang-Ma district of E2d
图 2 黄珏地区E2d1近岸水下冲积扇地震反射特征
Fig. 2. Near-shore subaqueous alluvial fans' seismic reflection character of E2d1 in HJ area
图 3 黄珏地区E2d1近岸水下冲积扇岩心沉积现象
a.黄3-3井，2 243.00 m，灰色砾岩，砾径可达10 cm以上，近岸水下冲积扇扇根；b.黄3-3井，2 239.00 m灰色含砾粗砂岩，颗粒支撑-杂基支撑近岸水下冲积扇扇中主水道；c.新黄31井，2 715.00 m灰色粗砂岩，偶见定向排列泥砾，近岸水下冲积扇扇中辫状水道；d.黄31井，2 369.00 m灰白色泥质粉砂岩-砂质泥岩，近岸水下冲积扇扇中辫状水道；e.黄32井，2 365.00 m灰白色粉砂岩与灰色泥岩互层，近岸水下冲积扇扇中水道间；f.黄31井，2 239.00 m灰褐色泥岩，含植物叶片化石，近岸水下冲积扇扇端
Fig. 3. Core sedimentary phenomenon of E2d1 in HJ area
图 4 黄32井E2d1近岸水下冲积扇沉积局部
Fig. 4. Part of near-shore subaqueous alluvial Fans profile in well H32, E2d1
图 5 黄珏-马家嘴地区E2d2岩心沉积现象(从左至右表表示为从顶至底关系)
a.黄27-3井，1 555.00 m，棕红色泥岩差胶结，扇三角洲平原泥石流；b.黄35-2井，1 588.00 m，棕红色泥质粉砂岩见斜虫孔，扇三角洲平原辫状水道；c.黄4井，1 511.82 m，棕红色粉砂质泥岩, 扇三角平原分流间湾；d.黄4井，1 878.00 m，杂色含砾不等粒砂岩，扇三角洲前缘水下主水道底部；e.马6井，1 572.00 m，灰白色砾质粗砂岩，扇三角洲前缘水道；f.黄4井，1 876.00 m，杂色砾岩向上变为灰色粗砂岩，扇三角洲前缘水下河道；g.马6井，1 569.01 m，棕色-黄绿色泥岩互层见波状层理，扇三角洲前缘水下天然堤；h.马7井，1 477.00 m，灰绿色粉砂质泥岩与褐色泥岩互层见人字形交错层理，扇三角洲前缘席状砂；i.马7井，1 475.00 m，褐色油浸粗砂岩见楔状交错层理, 扇三角洲前缘水下分流河道
Fig. 5. Core sedimentary phenomenon of E2d2 in HJ-MJZ area
图 9 黄珏-马家嘴地区E2d1、E2d2滑塌-浊积岩岩心沉积现象(从左至右表表示为从顶至底关系
a.黄32井，2 372.78 m，E2d1，灰色粉砂岩-泥质粉砂岩，鲍马序列；b.马13-2井，1 439.53 m，E2d2，灰色泥质粉砂岩-粉砂质泥岩，泥质碎屑流；c.黄17-1井，1 511.82 m，E2d2，灰绿色砂质砾岩，砂质碎屑流；d.黄10井，1 535.34 m，E2d2，灰黄色砂质砾岩，砂质碎屑流(以上4照片由董桂玉2010年拍摄)
Fig. 9. Slump-turbidities cores of E2d in HJ-MJZ area
图 10 黄珏-马家嘴地区黄32井、马2井E2d1滑塌-浊积扇沉积
Fig. 10. Slump-turbidities profile of well H32 and well M2 in E2d1 in HJ-MJZ area
-
[1] Chen, A.D., 2001. Dynamic Mechanism of Formation of Dustpan Subsidence, Northern Jiangsu. Geological Journal of China Universities, 7(4): 409-418 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GXDX200104004.htm [2] Department of Geography, East China Normal University, 1984. Underwater Fan Characters of Well Ma4 in Gaoyou Sag, Eogene Dainan formation. Shanghai Geology, 2: 11-12 (in Chinese with English abstract). [3] Dong, R.X., Su, M.Z., 1985. Characteristic of Beachy Underwater Alluvial Fan Facies—With a Practical Example. Experimental Petroleum Geology, 7(4): 294-302 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYSD198504005.htm [4] Gao, L.K., Lin, C.M., Yao, Y.L., et al., 2010. Sedimentary Facies and Evolution of Paleogene Dainan Formation in Gaoyou Sag, Subei Basin. Acta Sedimentologica Sinica, 28(4): 706-716 (in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTotal-CJXB201004007.htm [5] Gilbert, G.K., 1885. The Topographic Features of Lake Shores. USGS Annual Report, 104-108. [6] Holmes, A., 1965. Principles of Physical Geology. The Ronald Press Co., New York, 1288. [7] Ji, Y.L., Li, Q.S., Wang, Y., et al., 2012. Fan Delta Sedimentary System and Facies Models of Dainan Formation of Paleocene in Gaoyou Sag. Journal of Earth Sciences and Environment, 34(1): 9-19 (in Chinese with English abstract). http://www.researchgate.net/publication/290130256_Fan_delta_sedimentary_system_and_facies_models_of_Dainan_Formation_of_Paleogene_in_Gaoyou_Sag [8] Jiang, Z.X., 2003. Sedimentology. Petroleum Industry Press, Beijing (in Chinese). [9] Li, L., 2010. Sedimentary Characteristics of the Fluxoturbidite of the Upper Submember of Sha 3 in Chexi Subsag. Journal of Xi'an Shiyou University(Natural Science Edition), 25(2): 22-25, 29 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-XASY201002007.htm [10] Ma, W.R., Fu, Q., Dong, G.Y., et al., 2012. Paleoenvironment Evolution and Sedimentary Characteristics of Dainan Formation in Gaoyou Sag. Journal of Tongji University(Natural Science), 40(3): 478-484 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-TJDZ201203026.htm [11] Qiu, X.M., Liu, Y.R., Fu, Q., 2006. Sequence Stratigraphy and Sedimentary Evolution of Upper Cretaceous-Tertiary in Northern Jiangsu Basin. Geological Publishing House, Beijing (in Chinese). [12] Shanmugam, G., 2008. Slides, Slumps, Debris Flows, and Turbidity Currents. In: Steele, J.H., Turekian, K.K., Thorpe, S.A., eds., Encyclopedia of Ocean Sciences. Elsevier, Amsterdam, 418. [13] Sun, Y.Z., Zhen, J.M., Wang, D.F., et al., 1980. Subaqueous Alluvial Fan—A New Field of Oil Exploration. Petroleum Geology & Experiment, 2(3): 32-41(in Chinese). [14] Wang, S.Q., 1993. Fan Delta Modles. Petroleum Industry Press, Beijing(in Chinese). [15] Wen, Q.Y., Zhang, C.B., Wu, P.K., 1990. Fan-Delta in an Evolving Basin. Journal of Changchun University of Earth Science, 20(4): 407-414(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CCDZ199004007.htm [16] Wu, C.Y., Xue, S.H., 1992. Sedimentology of Petroliferous Basins in China. Petroleum Industry Press, Beijing(in Chinese). [17] Xue, L.Q., Galloway, W.E., 1991. Fan-Delta, Braided River Delta and the Classification of Delta Systems. Acta Geologica Sinica, 65(2): 141-153(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE199102003.htm [18] Xue, L.Q., Xu, H.D., 1988. Sedimentary System of the Dainan Formation in Gaoyou Depression. Oil & Gas Geology, 9(3): 297-305(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYYT198803011.htm [19] Zhai, G.M., 1992. Petroleum Geology of China: Vol. 8. Petroleum Industry Press, Beijing (in Chinese). [20] Zhang, C.S., Liu, Z.B., Shi, D., et. al., 2000. Formed Proceeding and Evolution Disciplinarian of Fan Delta. Acta Sedimentologica Sinica, 18(4): 521-526 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-CJXB200004006.htm [21] Zhang, G.L., Chen, S.Y., Yan, J.H., et al., 2006. Simulation of Luxoturbidite in Front of Delta. Acta Sedimentologica Sinica, 24(1): 50-55(in Chinese with English abstract). http://www.researchgate.net/publication/285311989_Simulation_of_luxoturbidite_in_front_of_delta [22] Zhang, H.F., Tian, J.C., Zhang, T., et al., 2012. Characteristics and Genesis of Turbidite of Chang 6 and Chang 7 Oil Reservoirs in Huachg-Qingyang Area of Ordos Basin, China. Journal of Chengdu University of Technology (Science & Technology Edition), 39(3): 238-243 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CDLG201203003.htm [23] Zhang, J.L., Wang, B.Q., 1996. Facies Models for Lacustrine Fan Deltas in Hydrocarbon-Bearing Basins, China. Geological Review, 42(Suppl. ): 147-152(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DZLP1996S1021.htm [24] Zhang, J.L., Shen, F., 1991. Characteristics of Nearshore Subaqueous Fan Reservoir in Damoguaihe Formation, Wuerxun Depression. Acta Petrolei Sinica, 12(3): 25-35(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYXB199103003.htm [25] Zhang, M., Tian, J.C., 1999. The Nomenclature, Sedimentary Characteristics and Reservoir Potential of Nearshore Subaqueous Fans. Sedimentary Facies and Palaeogeography, 19(4): 42-52(in Chinese with English abstract). [26] Zhang, X.B., Zheng, R.C., Zhang, S.N., 2007. The Tectonic-Sedimentary System of the Dainan Formation in Majiazui-Lianmenzhuang Region, Gaoyou Sag. Petroleum Geology & Oilfield Development in Daqing, 26(1): 13-17(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQSK200701003.htm [27] Zhang, X.L., Zhu, X.M., Zhong, D.K., et al., 2005. Sedimentary Facies and Its Controlling on Subtle Oil and Gas Reservoirs of the Daina. Journal of Palaeogeography, 7(2): 207-218(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GDLX200502006.htm [28] Zhao, C.L., 2000. Sedimentary-Reservoir Geology Collection. Petroleum Industry Press, Beijing(in Chinese). [29] Zhu, X.M., Xin, Q.L., Liu, Z.R., 1991. Recognition of the Slump Turbidity Fan in Down-Faulted Lacustrine Basins. Chinese Science Bulletin, 36(7): 535-537(in Chinese). doi: 10.1360/csb1991-36-7-535 [30] 陈安定, 2001. 苏北箕状断陷形成的动力学机制. 高校地质学报, 7(4): 409-418. https://www.cnki.com.cn/Article/CJFDTOTAL-GXDX200104004.htm [31] 董荣鑫, 苏美珍, 1985. 近岸水下冲积扇相特征及实例. 石油实验地质, 7(4): 294-302. https://www.cnki.com.cn/Article/CJFDTOTAL-SYSD198504005.htm [32] 高丽坤, 林春明, 姚玉来, 等, 2010. 苏北盆地高邮凹陷古近系戴南组沉积相及沉积演化. 沉积学报, 28(4): 706-716. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201004007.htm [33] 华东师范大学地理系, 江苏油田沉积相研究组, 1984. 江苏高邮凹陷马4井下第三系戴南组水下扇的沉积特征. 上海地质, 2: 11-12. https://www.cnki.com.cn/Article/CJFDTOTAL-SHAD198402008.htm [34] 纪友亮, 李清山, 王勇, 等, 2012. 高邮凹陷古近系戴南组扇三角洲沉积体系及其沉积相模式. 地球科学与环境学报. 34(1): 9-19. doi: 10.3969/j.issn.1672-6561.2012.01.002 [35] 姜在兴, 2003. 沉积学. 北京: 石油工业出版社. [36] 李凌, 2010. 车西洼陷沙三上亚段滑塌浊积砂体的沉积特征. 西安石油大学学报(自然科学版), 25(2): 22-25, 29. doi: 10.3969/j.issn.1673-064X.2010.02.005 [37] 马文睿, 傅强, 董桂玉, 等, 2012. 高邮凹陷始新统戴南组古环境演化及沉积特征. 同济大学学报(自然科学版), 40(3): 478-484. doi: 10.3969/j.issn.0253-374x.2012.03.025 [38] 邱旭明, 刘玉瑞, 傅强, 2006. 苏北盆地上白垩统-第三系层序地层与沉积演化. 北京: 地质出版社. [39] 孙永传, 郑浚茂, 王德发, 等, 1980. 水下冲积扇——一个找油的新领域. 石油实验地质, 2(3): 32-41. https://www.cnki.com.cn/Article/CJFDTOTAL-SYSD198003007.htm [40] 王寿庆, 1993. 扇三角洲模式. 北京: 石油工业出版社. [41] 文琼英, 张川波, 吴培康, 1990. 盆地演化过程中的扇三角洲. 长春地质学院学报, 20(4): 407-414. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ199004007.htm [42] 吴崇筠, 薛叔浩, 1992. 中国含油气盆地沉积学. 北京: 石油工业出版社. [43] 薛良清, Galloway, W.E., 1991. 扇三角洲、辫状河三角洲与三角洲体系的分类. 地质学报, 65(2): 141-153. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE199102003.htm [44] 薛良清, 徐怀大, 1988. 苏北盆地高邮凹陷戴南组沉积体系. 石油与天然气地质, 9(3): 297-305. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT198803011.htm [45] 翟光明, 1992. 中国石油地质志: 卷八. 北京: 石油工业出版社. [46] 张春生, 刘忠保, 施冬, 等, 2000. 扇三角洲形成过程及演变规律. 沉积学报, 18(4): 521-526. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200004006.htm [47] 张关龙, 陈世悦, 鄢继华, 等, 2006. 三角洲前缘滑塌浊积体形成过程模拟. 沉积学报. 24(1): 50-55. doi: 10.3969/j.issn.1000-0550.2006.01.007 [48] 张海峰, 田景春, 张涛, 等, 2012. 花池-庆阳地区延长组长6-长7油层组浊积岩特征及成因. 成都理工大学学报(自然科学版). 39(3): 238-243. doi: 10.3969/j.issn.1671-9727.2012.03.002 [49] 张金亮, 沈凤, 1991. 乌尔逊凹陷大磨拐河组近岸水下扇储层特征. 石油学报, 12(3): 25-35. doi: 10.3321/j.issn:0253-2697.1991.03.001 [50] 张金亮, 王宝清, 1996. 我国含油气湖盆扇三角洲模式. 地质论评. 42(增刊): 147-152. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP1996S1021.htm [51] 张萌, 田景春, 1999. 近岸水下扇的命名、特征及其储集性. 岩相古地理, 19(4): 42-52. doi: 10.3969/j.issn.1009-3850.1999.04.005 [52] 张喜林, 朱筱敏, 钟大康, 等, 2005. 苏北盆地高邮凹陷古近系戴南组沉积相及其对隐蔽油气藏的控制. 古地理学报, 7(2): 207-218. doi: 10.3969/j.issn.1671-1505.2005.02.006 [53] 张小兵, 郑荣才, 张哨楠, 2007. 高邮凹陷马家嘴-联盟庄地区戴南组构造-沉积体系. 大庆石油地质与开发, 26(1): 13-17. doi: 10.3969/j.issn.1000-3754.2007.01.004 [54] 赵澄林, 2000. 沉积-储层地质文集. 北京: 石油工业出版社. [55] 朱筱敏, 信荃麟, 刘泽容, 1991. 陆相断陷湖盆中滑塌浊积扇的识别. 科学通报, 36(7): 535-537. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB199107016.htm -
下载:
点击查看大图
计量
- 文章访问数: 3003
- HTML全文浏览量: 133
- PDF下载量: 539
- 被引次数: 0
