歧口凹陷古近纪东营期古物源体系重建与应用

王华; 白云风; 黄传炎; 严德天; 刘彦博; 陈思; 向雪梅; 廖计华; 夏存银; 赵淑娥

歧口凹陷古近纪东营期古物源体系重建与应用

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

基金项目:

国家自然科学基金 40872077

湖北省自然科学重点基金 2008CDA098

详细信息

作者简介:
王华（1964—）, 男, 教授, 博士生导师, 研究方向为应用层序地层学、应用沉积学. E-mail：wanghua@cug.edu.cn

中图分类号: P618.13
计量
- 文章访问数: 3300
- HTML全文浏览量: 94
- PDF下载量: 50
- 被引次数: 0
出版历程
- 收稿日期: 2008-12-10
- 刊出日期: 2009-05-25

Reconstruction and Application of the Paleogene Provenance System of the Dongying Formation in Qikou Depression

Key L aboratory o f Tectonics and Petroleum Resources o f Ministry o f Education, Faculty of Earth Resources, China University o f Geosciences, Wuhan 430074, China

摘要

摘要: 以沉积盆地分析、层序地层研究和油气勘探实践中急待解决的古物源体系分析为切入点, 以歧口凹陷东营组研究为例, 阐述了古物源体系研究的途径、方法与技术路线; 初步总结出应用轻-重矿物时空配置关系、地震前积反射结构特征、古地貌恢复与沟谷展布特征、盆地内部骨架砂体形态与时空配置以及盆地边缘及内部层序界面上大型下切谷的空间展布特征, 即“五位合一”法来判断沉积盆地的古物源体系.该分析方法可为同领域的研究提供借鉴作用.
- 歧口凹陷 /
- 东营组 /
- 古物源体系
Abstract: The paleoprovenance system analysis is critical in terms of present sedimentary basin analysis, sequence stratigraphy study, and petroleum exploration practice.In this paper, we present a preliminarily summary of applying the "five-in-one" method to study provenace system of the Dongying Formation in the Qikou depression.The so-called "five-in-one" method is a compositive analysis of light-heavy minerals, seismic progradational reflection structure features, paleogeomorphy and gully expansion features, skeleton sand body forms within the basin and the time-space expansion and matching rules analysis, and basin margin and the spatial expansion features analysis of large-scale incised valley developed in its internal sequence boundary.This method undoubtedly provides a reference for the researches of other basins within the same field.However, we know that provenace analysis of sedimentary basin is a complicated job.With the development of science and technology, and the increase of basin data obtained, it will apply on the field together with more effective methods and technologies.It will also further approach the real status of provenace system, and provide better service for petroleum exploration.
- Qikou depression /
- Dongying Formation /
- Paleogene provenance system

HTML全文

图 1 歧口凹陷构造位置图(A、B为图 2、3地震剖面的位置)

Fig. 1. Tectonic location map of Qikou depression

下载: 全尺寸图片幻灯片

图 2 歧口凹陷SN向构造剖面图

(剖面位置见图 1)

Fig. 2. Seismic profile from north to south in Qikou depression

下载: 全尺寸图片幻灯片

图 3 歧口凹陷NW-SE向构造剖面图

(剖面位置见图 1)

Fig. 3. Seismic profile from northwest to southeast in Qikou depression

下载: 全尺寸图片幻灯片

图 4 歧口凹陷东营组重矿物(a) 和轻矿物(b) 组分分析

(据白云风等, 2006修改)

Fig. 4. Analysis of the heavy minerals (a) and the light minerals (b) of Dongying Formation in Qikou depression

下载: 全尺寸图片幻灯片

图 5 地震前积反射特征与物源供给系统

Fig. 5. Characteristic of progradational reflection and the supplying system of provenance

下载: 全尺寸图片幻灯片

图 6 歧口凹陷东营组同沉积期古地貌与物源体系分析

Fig. 6. Analysis of paleogeomorphy and provenance of Dongying Formation in Qikou depression

下载: 全尺寸图片幻灯片

图 7 歧口凹陷东营组砂体厚度图

Fig. 7. Isopach map of Dongying Formation in Qikou depression

下载: 全尺寸图片幻灯片

图 8 歧口凹陷东营组下切谷地震反射特征

Fig. 8. Seismic reflection characteristic of incise valley of Dongying Formation in Qikou depression

下载: 全尺寸图片幻灯片

图 9 歧口凹陷东营组物源方向综合分析

Fig. 9. Provenance analysis of the Dongying Formation in Qikou depression

下载: 全尺寸图片幻灯片

参考文献(41)

[1]	Bai, Y. F., Wang, Z. S., Wei, A. J., et al., 2008. Time andspace distribution characteristics and material resourcesystem of heavy minerals in Dongying Formation of Huanghua depression. Petroleum Geology & Oilfield Development in Daqing, 27 (2): 39-42 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQSK200802010.htm
[2]	Bai, Y. F., Zhang, B., Wang, H., et al., 2006. Research onthe source direction of Palaeogene Dongying Formationin Huanghua depression. Journal of Oil and Gas Tech-nology, 28 (3): 17-19 (in Chinese with Englishabstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-JHSX200603004.htm
[3]	Bonjour, J. L., Dabard, M. P., 1990. Ti/Nb ratios of clasticterrigenous sediments used as an indicator of prove-nance. Chemical Geology, 91 (3): 257-267. http://www.researchgate.net/profile/Marie_Pierre_Dabard/publication/222866389_TiNb_ratios_of_clastic_terrigenous_sediments_used_as_an_indicator_of_provenance/links/54ff356f0cf2eaf210b7ad53.pdf
[4]	Chen, C. F., Zheng, J. M., Wang, D. F., 2001. Depositionalsystems and source provenance of the third member of Shahejie Formation in Banqiao sag. Journal of Palaeo-geography, 3 (1): 55-62 (in Chinese with Englishabstract). http://en.cnki.com.cn/Article_en/ http://search.cnki.net/down/default.aspx?filename=GDLX200101005&dbcode=CJFD&year=2001&dflag=pdfdown
[5]	Deng, H. W., Wang, H. L., Wang, D. Z., 2001. Control of paleo-morphology to stratigraphic sequence in continental rift basins: Take Lower Tertiary of western slope in Bozhong depression as an example. Oil and Gas Geology, 22 (4): 293-296, 303 (in Chinese with Englishabstract). http://en.cnki.com.cn/article_en/cjfdtotal-syyt200104001.htm
[6]	Dickinson, W. R., 1985. Interpreting provenance relations from detrital modes of sandstones. In: Zuffa, G. G., ed., Provenance of arenites. NATO-ASI Series. D. Reidel., Dordrecht, 148: 333-361.
[7]	Haughton, P. D. W., Morton, A. C., Todd, S. P., 1991. Developments in sedimentary provenance studies. The Geological Society of London, London.
[8]	He, Z. H., Liu, Z. J., Zhang, F., 2001. Latest progress ofheavy mineral researchin the basin analysis. Geological Science and Technology Information, 20 (4): 29-32 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-DZKQ200104007.htm
[9]	Jiao, Y. Q., Li, Z., Zhou, H. M., 1998. The integrated studyof sediment sources in sedimentary basins: An examplefromthe Eocene Nanpu rift subbasin. Sedimentary Facies and Palaeogeography, 18 (5): 16-20 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YXGD805.002.htm
[10]	Johnson, C. M., Winter, B. L., 1999. Provenance analysis of Lower Paleozoic cratonic quartz arenites of the North American midcontinent region: U-Pb and Sm-Nd isotope geochemistry. Geological Society of American Bulletin, 111 (11): 1723-1738. doi: 10.1130/0016-7606(1999)111<1723:PAOLPC>2.3.CO;2
[11]	Li, Z., Jiao, Y. Q., Liu, C. H., et al., 1998. Source analysis ofheavy mineral in Gaoliu area, Huanghua depression. Petroleum Exploration and Development, 25 (6): 5-7 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SKYK806.001.htm
[12]	Lin, C. S., 2006. Tectono-stratigraphic analysis of sedimenta-ry basins: Acase study on the inland tectonically activebasins in China. Geoscience, 20 (2): 185-194 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-XDDZ200602000.htm
[13]	Liu, L., Hu, C. Y., 1991. Provenance significance of the maindetrital composition in sandstone. Sedimentary Faciesand Palaeogeography, 11 (6): 48-53 (in Chinese with English abstract).
[14]	McLennan, S. M., Hemming, S., McDaniel, D. K., et al., 1993. Geochemical approaches to sedimentation, prove-nance, and tectonics. Special Paper-Geological Societyof America, 284: 21-40. http://ci.nii.ac.jp/naid/10010160942
[15]	Morton, A., Hurst, A., 1995. Correlation of sandstonesusing heavy minerals: An example from the Statfjord Formation of the Snorre Field, northern North Sea. In: Dunay, R. E., Hail wood, E. A., eds., Non-biostrati-graphical methods of dating and correlation. Geological Society Special Publication, 89: 3-22.
[16]	Ravnas, R., Steel, R. J., 1998. Architecture of marine rift-ba-sin successions. AAPG Bulletin, 82: 110-146. http://www.onacademic.com/detail/journal_1000040838097510_1c38.html
[17]	Sambridge, M. S., Compston, W., 1994. Mixture modeling ofmulti-component data sets with application to ion-probezircon ages. Earthand Planetary Science Letters, 128 (3-4): 373-390. doi: 10.1016/0012-821X(94)90157-0
[18]	Sherlock, S. C., Jones, K. A., Jones, J. A., 2000. A Central European variscide source for Upper Carboniferous sed-iments in SW England: ⁴⁰Ar/³⁹Ar detrital white micaages fromthe Forest of Dean basin. Journal ofthe Geological Society, 157 (5): 905-908. doi: 10.1144/jgs.157.5.905
[19]	Stevenson, R. K., Whittaker, S., Mountjoy, E. W., 2000. Ge-ochemical and Nd isotopic evidence for sedimentary-source changes in the Devonian miogeocline of thesouthern Canadian Cordillera. Geological Society of American Bulletin, 112: 531-539. doi: 10.1130/0016-7606(2000)112<531:GANIEF>2.0.CO;2
[20]	Taylor, S. R., McLennan, S. M., 1985. The continentalcrust: Its composition and evolution. Blackwell Scientific Publication, Oxford.
[21]	Wang, J. H., Wang, H., Zhao, Z. X., et al., 2003. Sequence stratigraphy in paleogeomorphy analysis: An examplefrom Tahe oilfield. Earth Science-Journal of China University of Geosciences, 28 (4): 425-430 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx200304011
[22]	Wang, Z. J., Chen, H. D., Zhang, J. Q., 2000. The researchand prospect in provenance analysis. Sedimentary Geology and Tethyan Geology, 20 (4): 104-110 (in Chinese with English abstract). http://www.researchgate.net/publication/291867287_The_research_and_prospect_in_provenance_analysis
[23]	Wang, Z. Y., Qi, J. F., Lu, K. Z., 2000. Analysis of Cenozoictectonic subsidence history of the east tectonic belts in Huanghua depression. Oil and Gas Geology, 21 (2): 127-129, 167 (in Chinese with English abstract). http://www.researchgate.net/publication/284481133_Analysis_of_Cenozoic_tectonic_subsidence_history_of_the_east_tectonic_belts_in_Huanghua_Depression
[24]	Yan, Y., Lin, G., Wang, Y. J., et al., 2002. The indication ofcontinental detrital sediment to tectonic setting. Advance in Earth Sciences, 17 (1): 85-90 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXJZ200201012.htm
[25]	Zhang, J. L., Lin, C. S., Zheng, H. R., 2002. Controlling ac-tion of fractures, palaeogeomorphology and materialsources of rift lake basin on sedimentary system-Taking E_s3 Gubei subsag as example. Petroleum Geologyand Recovery Efficiency, 9 (4): 24-27 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YQCS200204009.htm
[26]	Zhao, J. X., Chen, H. D., Shi, Z. Q., 2001. The way and implications of rebuilding palaeogeomorphology, taking theresearch of palaeogeomorphology of the Ordos basin before Jurassic deposition as example. Journal of Chengdu University of Technology, 28 (3): 260-266 (in Chinese with English abstract). http://www.researchgate.net/publication/279557155_The_way_and_implications_of_rebuilding_palaeogeomorphology
[27]	白云风, 王振升, 韦阿娟, 等, 2008. 黄骅坳陷东营组重矿物时空展布特征及物源体系分析. 大庆石油地质与开发, 27 (2): 39-42. doi: 10.3969/j.issn.1000-3754.2008.02.011
[28]	白云风, 张兵, 王华, 等, 2006. 黄骅坳陷古近纪东营组物源方向研究. 石油天然气学报, 28 (3): 17-19. doi: 10.3969/j.issn.1000-9752.2006.03.005
[29]	陈纯芳, 郑浚茂, 王德发, 2001. 板桥凹陷沙三段沉积体系与物源分析. 古地理学报, 3 (1): 55-62. doi: 10.3969/j.issn.1671-1505.2001.01.006
[30]	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
[31]	和钟铧, 刘招君, 张峰, 2001. 重矿物分析在盆地中的应用研究进展. 地质科技情报, 20 (4): 29-32. doi: 10.3969/j.issn.1000-7849.2001.04.006
[32]	焦养泉, 李珍, 周海民, 1998. 沉积盆地物质来源综合研究—以南堡老第三纪亚断陷盆地为例. 岩相古地理, 18 (5): 16-20. https://www.cnki.com.cn/Article/CJFDTOTAL-TTSD199805005.htm
[33]	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
[34]	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
[35]	刘立, 胡春燕, 1991. 砂岩中主要碎屑成分的物源区意义. 岩相古地理, 11 (6): 48-53. https://www.cnki.com.cn/Article/CJFDTOTAL-TTSD199106006.htm
[36]	王家豪, 王华, 赵忠新, 等, 2003. 层序地层学应用于古地貌分析—以塔河油田为例. 地球科学—中国地质大学学报, 28 (4): 425-430. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200304011.htm
[37]	汪正江, 陈洪德, 张锦泉, 2000. 物源分析的研究与展望. 沉积与特提斯地质, 20 (4): 104-110. doi: 10.3969/j.issn.1009-3850.2000.04.011
[38]	王子煜, 漆家福, 陆克政, 2000. 黄骅坳陷东部构造带新生代构造沉降史分析. 石油与天然气地质, 21 (2): 127-129, 167. doi: 10.3321/j.issn:0253-9985.2000.02.008
[39]	闫义, 林舸, 王岳军, 等, 2002. 盆地陆源碎屑沉积物对源区构造背景的指示意义. 地球科学进展, 17 (1): 85-90. doi: 10.3321/j.issn:1001-8166.2002.01.013
[40]	张建林, 林畅松, 郑和荣, 2002. 断裂湖盆断裂、古地貌及物源对沉积体系的控制作用—以孤北洼陷沙三段为例. 油气地质与采收率, 9 (4): 24-27. doi: 10.3969/j.issn.1009-9603.2002.04.009
[41]	赵俊兴, 陈洪德, 时志强, 2001. 古地貌恢复技术方法及其研究意义—以鄂尔多斯盆地侏罗纪沉积前古地貌研究为例. 成都理工学院学报, 28 (3): 260-266. doi: 10.3969/j.issn.1671-9727.2001.03.008