北塘凹陷古近系沙河街组三段物源体系分析

黄传炎; 王华; 周立宏; 任培罡; 刘军; 白云风

北塘凹陷古近系沙河街组三段物源体系分析

黄传炎^{1, 2,},
王华^{1, 2},
周立宏³,
任培罡^{1, 2},
刘军^{1, 2},
白云风^{1, 2}

1.
中国地质大学资源学院, 构造与油气资源教育部重点实验室，湖北武汉 430074
2.
中国地质大学地质过程与矿产资源国家重点实验室，湖北武汉 430074
3.
中国石油大港油田公司勘探开发研究院，天津 300280

基金项目:

国家自然科学基金项目 40872077

中国地质大学(武汉) 地质过程与矿产资源国家重点实验室开放课题基金 GPMR200913

构造与油气资源教育部重点实验室开放基金 TPR-2009-19

详细信息

作者简介:
黄传炎(1976-), 男, 博士, 主要从事层序地层学和沉积学研究.E-mail: cyhuang76@163.com

中图分类号: P588.21;P539.4
计量
- 文章访问数: 3798
- HTML全文浏览量: 898
- PDF下载量: 67
- 被引次数: 0
出版历程
- 收稿日期: 2008-12-15
- 刊出日期: 2009-11-25

Provenance System Characters of the Third Member of Shahejie Formation in the Paleogene in Beitang Sag

HUANG Chuan-yan^{1, 2
,},
WANG Hua^{1, 2},
ZHOU Li-hong³,
REN Pei-gang^{1, 2},
LIU Jun^{1, 2},
BAI Yun-feng^{1, 2}

1.
Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China
3.
Research Institute of Exploration and Development, PetroChina Dagang Oilfield Company, Tianjin 300280, China

摘要

摘要: 物源分析是盆地分析的重要内容之一.北塘凹陷古近系沙河街组三段(Es₃) 湖泊范围广、沉积厚度大, 而勘探程度低, 是大港油田未来勘探的重要突破区, 精细刻画北塘凹陷沙三段物源体系对沉积体系重建、有利区带预测具有重要意义.采用构造格架及古地貌宏观区分物源区与沉积区, 根据碎屑矿物组合特征划分物源区块, 依据地震反射特征勾绘物源在盆内进积方向, 利用砂体等厚图和砂地比等值线图精细描绘物源分支, 从不同角度、不同层次对北塘凹陷沙三段古物源体系进行精细研究.结果表明, 北塘凹陷物源来自北部燕山褶皱带和西部沧县隆起, 具体分为西部的沧县物源、西北角的汉沽物源、北部的大神堂物源和东北角的涧南物源.在物源体系和构造组合特征的控制下, 沙三段主要发育扇三角洲沉积体系.
- 物源分析 /
- 沉积体系 /
- 沉积作用 /
- 北塘凹陷 /
- 沙三段
Abstract: Provenance analysis is an important aspect of basin analysis. Beitang sag is an important breakthrough zone for future exploration in Dagang oilfield with its wide range of lake, deep sediment thickness, and low level of exploration of the third member of Shahejie Formation (Es₃). Detailed depiction of the provenance system using of Es₃ is of practical significance for reconstructing depositional system and forecasting favorable areas. This paper analyzes in detail the provenance system of Es₃ in Beitang sag from various angles and levels: the source area and the deposition area is macroscopically distinguished according to tectonic framework and palaeogeomorphology; the source block is determined according to the characteristics of detrital mineral assemblage; the direction of transporting clastic fragmen in the basin is described according to seismic reflection characteristics; and the source branches are finely pictured according to sandstone thickness distribution map and percent distribution map The research results show that provenances originated from Yanshan fold belt and Cangxian uplift. They are divided into western Cangxian source, north-west Hangu source, north Dashentang source and north-east Jiannan source. In the tectonic framework and the provenance system, there mainly developed fan-delta depositional system of Es₃ in Beitang sag.
- provenance analysis /
- sedimentation system /
- sedimentology /
- Beitang sag /
- the third member of Shahejie Formation

HTML全文

图 1 北塘凹陷区域地质和构造格架(据大港资料修改, 2004)

Fig. 1. Regional geological map and structure framework of Beitang sag

下载: 全尺寸图片幻灯片

图 2 北塘凹陷沙三段发育初期古地貌图与物源体系匹配

Fig. 2. The palaeogeomorphology and provenance system of Es₃ in Beitang sag

下载: 全尺寸图片幻灯片

图 3 北塘凹陷沙三段轻重矿物分析

Fig. 3. Light and heavy mineral combination characteristic analysis of Es₃ in Beitang sag

下载: 全尺寸图片幻灯片

图 4 地震反射特征分析

Fig. 4. Provenance analysis of seismic character

下载: 全尺寸图片幻灯片

图 5 北塘凹陷沙三一亚段砂岩百分率平面分布

Fig. 5. Sandstone percent map of Es₃¹ in Beitang sag

下载: 全尺寸图片幻灯片

图 6 北塘凹陷沙三一亚段沉积体系空间展布

SP.自然电位, mV; Rt.视电阻率, Ω·m

Fig. 6. Sedimentary system distribution map of Es₃¹ in Beitang sag

下载: 全尺寸图片幻灯片

图 7 北塘凹陷沙三段古地貌、物源及沉积相综合分析

Fig. 7. The palaeogeomorphology, provenance analysis and sedimentary system distribution map of Es₃ in Beitang sag

下载: 全尺寸图片幻灯片

参考文献(48)

Deng, H. W., Guo, J. Y., Wang, R. J., et al., 2008. Tectonic sequence stratigraphic analysis in continental faulted basins. Earth Science Frontiers, 15 (2): 1-7 (in Chinese with English abstract). doi: 10.1016/S1872-5791(08)60024-X
Deng, H. W., Wang, H. L., Wang, D. Z., 2001. Control of palaeomorphology to stratigraphic sequencein continental rift basins: Take Lower Tertiary of western slope in Bozhong depression as an example. Oil & Gas Geology, 22 (4): 293-296, 303 (in Chinese with English abstract).
Deng, R. J., Xu, B., Qi, J. F., et al., 2005. Petroleum geological role of Paleogene overpressure reservoirs in Tanggu-Xincun of Beitang sag, Bohai Bay basin. Petroleum Exploration and Development, 32 (6): 46-51 (in Chinese with English abstract).
Deng, R. J., Xu, B., Qi, J. F., et al., 2006. Sedimentation characteristics and factors affecting the reservoir in Palaeogene the Shasan Member of Beitang sag, Huanghua depression. Acta Petrologica et Mineralogica, 25 (3): 230-236 (in Chinese with English abstract).
Emmel, B., Geiger, M., Jacobs, J., 2006. Detrital apatite fission-track ages in Middle Jurassic strata at the rifted margin of W Madagascar: Indicator for a protracted resedimentation history. Sedimentary Geology, 186 (1-2): 27-38. doi: 10.1016/j.sedgeo.2005.09.022
Huang, C. Y., Wang, H., Xiao, D. Q., et al., 2007. Sequence patterns, characteristics of depositional systems and model of reservoirs of fault steep slope selt of the first member of Shahejie Formation in Banqiao Sag. Acta Sedimentologica Sinica, 25 (3): 386-391 (in Chinese with English abstract).
Jiang, Z. X., 2003. Sedimentology. Petroleum Industry Press, Beijing (in Chinese).
Li, C., Cao, Q. B., Shou, J. F., et al., 2009. Application of fractal dimension of natural gamma logging curve in provenance analysis—A case in lower member of Ganchaigou Formation, Qigequan-Shibei area, Qaidam Basin. Natural Gas Geoscience, 20 (1): 148-152 (in Chinese with English abstract).
Li, P. L., Cai, J. G., Wang, J. F., et al., 2003. Petroleum geology and exploration of continental fault basin (Volume Ⅱ) -Sedimentary systemand hydrocarbon distribution of continental fault basin. Petroleum Industry Press, Beijing (in Chinese).
Li, S. T., Lu, F. X., Lin, C. S., 1997. The evolution of basin and the backgrounds of geodynamics in circum pacific ocean in eastern China during Mesozoic and Cenozoic. China University of Geosciences Press, Wuhan (in Chinese).
Li, S. T., Pan, Y. L., Lu, Y. C., et al., 2002. Key technology of prospecting and exploration of subtle traps in lacustrine fault basins: Sequence stratigraphic researches on the basis of high resolution seismic survey. Earth Science—Journal of China University of Geosciences, 27 (5): 593-598 (in Chinese with English abstract).
Li, Z., Jiao, Y. Q., Liu, C. H., et al., 1998. Source analysis of heavy mineral in Gaoliu area of Huanghua depression. Petroleum Exploration and Development, 25 (6): 5-7 (in Chinese with English abstract).
Lin, C. S., 2006. Tectonic-stratigraphic analysis of sedimentary basins: A case study on the inland tectonically active basins in China. Geoscience, 20 (2): 185-194 (in Chinese with English abstract).
Lin, C. S., Zheng, H. R., Ren, J. Y., et al., 2004. The control of syndepositional faulting on the Eogene sedimentary basin fills of the Dongying and Zhanhua sags, Bohai Bay rift basin. Science in China (Series D), 47 (9): 769-782. doi: 10.1360/03yd0203
Liu, S. F., Zhang, G. W., Zhang, Z. Q., et al., 2001. Isotopic geochronology tracer of the conglomerate from granite rock in Hefei basin. Chinese Science Bulletin, 46 (9): 748-753 (in Chinese with English abstract). doi: 10.1360/csb2001-46-9-748
Lu, Z. Y., 2008. Influence of the Paleogene structural styles on deposition and reservoir in Chezhen sag, Bohai Bay basin. Journal of Palaeography, 10 (3): 277-285 (inChinese with English abstract).
Wang, S. H., Jiao, Y. Q., Wu, L. Q., et al., 2007. Spatial combination of paleoprovenance and depositional lobe of mid-lower Yanchang Formationin the northwest of Ordos basin. Earth Science—Journal of China University of Geosciences, 32 (2): 201-208 (in Chinese with English abstract).
Wu, F. D., Lu, Y. C., Ruan, X. Y., 1996. Application of heavy minerals cluster analysis to study of clastic sources and stratigraphic correlation. Geoscience, 10 (3): 397-403 (in Chinese with English abstract).
Wu, L., Xu, H. M., Ji, H. C., 2006. Evolution of sedimentarysy stemand analysis of sedimentary source in Paleogene of Bozhong sag, Bohai Bay. Marine Geology & Quaternary Geology, 26 (1): 81-88 (in Chinese with English abstract).
Xiao, K. Y., Deng, R. J., Yang, H., et al., 2004. Petroleum geological role of magmatic activities in Xingang prospect area, Beitang sag. Petroleum Exploration and Development, 31 (2): 25-28 (in Chinese with English abstract).
Xu, T. W., Song, H. Q., Kuang, H., et al., 2009. Synthetic application of the provenance analysis technique: A case study of memberⅠof Taizhou Formation in Gaoyou sag, Subei basin. Acta Geoscientica Sinica, 2 (15): 111-117 (in Chinese with English abstract).
Yu, Z. H., Yang, C. Y., Liao, Q. J., et al., 1997. Natural gas geology of Huanghua depression. Petroleum Industry Press, Beijing (in Chinese).
Zhao, H. G., Liu, C. Y., 2003. Approaches and prospects of provenance analysis. Acta Sedimentologica Sinica, 21 (3): 409-415 (in Chinese with English abstract).
Zhou, H. M., Wang, Z. C., Guo, Y. H., et al., 2000. Tectonic controls on sequence stratigraphy in Tertiary Period in Nanbao depression. Journal of China University of Mining & Technology, 29 (3): 326-330 (in Chinesewith English abstract).
Zhou, Z. Y., Liao, Z. T., Yang, F. L., et al., 2001. Fissiontrack analysis and its application in the study of sedimentary basins. Petroleum Geology & Experiment, 23 (3): 332-337 (in Chinese with English abstract).
邓宏文, 郭建宇, 王瑞菊, 等, 2008. 陆相断陷盆地的构造层序地层分析. 地学前缘, 15 (2): 1-7. doi: 10.3321/j.issn:1005-2321.2008.02.001
邓宏文, 王红亮, 王敦则, 2001. 古地貌对陆相裂谷盆地层序充填特征的控制: 以渤中凹陷西斜坡区下第三系为例. 石油与天然气地质, 22 (4): 293-296, 303. doi: 10.3321/j.issn:0253-9985.2001.04.002
邓荣敬, 徐备, 漆家福, 等, 2005. 北塘凹陷塘沽-新村地区古近系异常高压特征及其石油地质意义. 石油勘探与开发, 32 (6): 46-51. doi: 10.3321/j.issn:1000-0747.2005.06.011
邓荣敬, 徐备, 漆家福, 等, 2006. 北塘凹陷古近系沙河街组三段沉积特征及储层的影响因素. 岩石矿物学杂志, 25 (3): 230-236. doi: 10.3969/j.issn.1000-6524.2006.03.008
黄传炎, 王华, 肖敦清, 等, 2007. 板桥凹陷断裂陡坡带沙一段层序样式和沉积体系特征及其成藏模式研究. 沉积学报, 25 (3): 386-391. doi: 10.3969/j.issn.1000-0550.2007.03.009
姜在兴, 2003. 沉积学. 北京: 石油工业出版社
李昌, 曹全斌, 寿建峰, 等, 2009. 自然伽马曲线分形维数在沉积物源分析中的应用———以柴达木盆地七个泉-狮北地区下干柴沟组下段为例. 天然气地球科学, 20 (1): 148-152. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX200901027.htm
李丕龙, 蔡进功, 王居峰, 等, 2003. 陆相断陷盆地油气地质与勘探———陆相断陷盆地沉积体系与油气分布(Ⅱ). 北京: 石油工业出版社.
李思田, 路风香, 林畅松, 1997. 中国东部及邻区中、新生代盆地演化及地球动力学背景. 武汉: 中国地质大学出版社.
李思田, 潘元林, 陆永潮, 等, 2002. 断陷湖盆隐蔽油气藏预测及勘探的关键技术———高精度地震探测基础上的层序地层学研究. 地球科学———中国地质大学学报, 27 (5): 592-598. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200205018.htm
李珍, 焦养泉, 刘春华, 等, 1998. 黄骅坳陷高柳地区重矿物物源分析. 石油勘探与开发, 25 (6): 5-7. doi: 10.3321/j.issn:1000-0747.1998.06.002
林畅松, 2006. 沉积盆地的构造地层分析———以中国构造活动盆地研究为例. 现代地质, 20 (2): 185-194. doi: 10.3969/j.issn.1000-8527.2006.02.001
刘少峰, 张国伟, 张宗清, 等, 2001. 合肥盆地花岗岩砾石的同位素年代学示踪. 科学通报, 46 (9): 748-753. doi: 10.3321/j.issn:0023-074X.2001.09.010
路智勇, 2008. 渤海湾盆地车镇凹陷古近系构造样式对沉积及储集层的影响. 古地理学报, 10 (3): 277-285. https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX200803011.htm
王世虎, 焦养泉, 吴立群, 等, 2007. 鄂尔多斯盆地西北部延长组中下部古物源与沉积体空间配置. 地球科学———中国地质大学学报, 32 (2): 201-208. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200702006.htm
武法东, 陆永潮, 阮小燕, 1996. 重矿物聚类分析在物源分析及地层对比中的应用———以东海陆架盆地西湖凹陷平湖地区为例. 现代地质, 10 (3): 397-403. https://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ603.014.htm
吴磊, 徐怀民, 季汉成, 2006. 渤海湾盆地渤中凹陷古近系沉积体系演化及物源分析. 海洋地质与第四纪地质, 26 (1): 81-88. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200601018.htm
肖坤叶, 邓荣敬, 杨桦, 等, 2004. 北塘凹陷新港探区新生代岩浆活动的石油地质意义. 石油勘探与开发, 31 (2): 25-28. doi: 10.3321/j.issn:1000-0747.2004.02.006
徐田武, 宋海强, 况昊, 等, 2009. 物源分析方法的综合运用———以苏北盆地高邮凹陷泰-段地层为例. 地球学报, 2 (15): 111-117. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB200901019.htm
于志海, 杨池银, 廖前进, 等, 1997. 黄骅坳陷天然气地质. 北京: 石油工业出版社.
赵红格, 刘池洋, 2003. 物源分析方法及研究进展. 沉积学报, 21 (3): 409-415. doi: 10.3969/j.issn.1000-0550.2003.03.007
周海民, 汪泽成, 郭英海, 等, 2000. 南堡凹陷第三纪构造作用对层序地层的控制. 中国矿业大学学报, 29 (3): 326-330. doi: 10.3321/j.issn:1000-1964.2000.03.025
周祖翼, 廖宗廷, 杨凤丽, 等, 2001. 裂变径迹分析及其在沉积盆地研究中的应用. 石油实验地质, 23 (3): 332-337. doi: 10.3969/j.issn.1001-6112.2001.03.015