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    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

    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, 2009. 歧口凹陷古近纪东营期古物源体系重建与应用. 地球科学, 34(3): 448-456.
    引用本文: 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, 2009. 歧口凹陷古近纪东营期古物源体系重建与应用. 地球科学, 34(3): 448-456.
    WANG Hua, BAI Yun-feng, HUANG Chuan-yan, YAN De-tian, LIU Yan-bo, CHEN Si, XIANG Xue-mei, LIAO Ji-hua, XIA Cun-yin, ZHAO Shu-e, 2009. Reconstruction and Application of the Paleogene Provenance System of the Dongying Formation in Qikou Depression. Earth Science, 34(3): 448-456.
    Citation: WANG Hua, BAI Yun-feng, HUANG Chuan-yan, YAN De-tian, LIU Yan-bo, CHEN Si, XIANG Xue-mei, LIAO Ji-hua, XIA Cun-yin, ZHAO Shu-e, 2009. Reconstruction and Application of the Paleogene Provenance System of the Dongying Formation in Qikou Depression. Earth Science, 34(3): 448-456.

    歧口凹陷古近纪东营期古物源体系重建与应用

    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

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

    • 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.

       

    • 图  1  歧口凹陷构造位置图(AB图 23地震剖面的位置)

      Fig.  1.  Tectonic location map of Qikou depression

      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

      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

      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

      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

      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

      图  7  歧口凹陷东营组砂体厚度图

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

      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

      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

    • 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
      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
      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
      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
      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
      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.
      Haughton, P. D. W., Morton, A. C., Todd, S. P., 1991. Developments in sedimentary provenance studies. The Geological Society of London, London.
      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
      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
      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
      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
      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
      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).
      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
      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.
      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
      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
      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
      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
      Taylor, S. R., McLennan, S. M., 1985. The continentalcrust: Its composition and evolution. Blackwell Scientific Publication, Oxford.
      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
      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
      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
      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
      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 Es3 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
      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
      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
      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
      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
      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
      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
      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
      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
      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
      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
      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
      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
      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
      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
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    • 收稿日期:  2008-12-10
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