南堡凹陷老爷庙地区构造-沉积分析

张翠梅; 刘晓峰; 苏明

Volume 34 Issue 5

Sep. 2009

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Article Navigation > Earth Science > 2009 > 34(5): 829-834

ZHANG Cui-mei, LIU Xiao-feng, SU Ming, 2009. Tectono-Sedimentary Analysis of Laoyemiao Region in Nanpu Depression. Earth Science, 34(5): 829-834.

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ZHANG Cui-mei, LIU Xiao-feng, SU Ming, 2009. Tectono-Sedimentary Analysis of Laoyemiao Region in Nanpu Depression. Earth Science, 34(5): 829-834.

ZHANG Cui-mei, LIU Xiao-feng, SU Ming, 2009. Tectono-Sedimentary Analysis of Laoyemiao Region in Nanpu Depression. Earth Science, 34(5): 829-834.

Citation:

ZHANG Cui-mei, LIU Xiao-feng, SU Ming, 2009. Tectono-Sedimentary Analysis of Laoyemiao Region in Nanpu Depression. Earth Science, 34(5): 829-834.

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Tectono-Sedimentary Analysis of Laoyemiao Region in Nanpu Depression

ZHANG Cui-mei^{1, 2
,},
LIU Xiao-feng^{1, 2},
SU Ming^{1, 2}

1.
Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences, Wuhan 430074, China
2.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2009-01-21
Publish Date: 2009-09-25

Abstract

Abstract

The aim of this paper is to test a new approach-tectono-sedimention analysis to gain insights into the controls of Laoyemiao transverse fold on the fan delta of Dongying Formation.By investigating the features of basin-bounding master fault (Xi'nanzhuang fault) and fold geometry in Laoyemiao region, we have determined that Laoyemiao fold is essentially a transverse fold produced by Xi'nanzhuang fault flexural.The fold with axes trending NW-SE was developed in sedimentary period of the 1 st Member of Shahejie Fm., and superimposed by Miocene NE trending strike-slip faults.Calculation of gravel content shows that the high values zone basically coincides with the hinge, which in turn reveals that the joint of the transverse fold and Xi'nanzhuang fault is the main drainage entry, and fold hinge provides major sediment long distance transportation pathway.From logging, seismic data and paleogeomorphology, the upper and lower slope break of transverse fold are identified.The sedimentary facies interpretation shows that they are consistent with the delimits of fan-delta plain and front, fan-delta front and pro-fan delta respectively.It can be proved that transverse fold constrains the facies distribution.Transverse folds caused by basin-bounding master fault are widely developed in sedimentary basins.The established model of sediment transportation for long distance and facies distribution of transverse fold is significant for favorable sandbodies prediction.
- transverse fold,
- tectono-sedimention analysis,
- Laoyemiao region,
- Nanpu Depression

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References

Blair, T. C., McPherson, J. G., 1994. Alluvial fans and theirnatural distinction from rivers based on morphology, hydraulic processes, sedimentary processes, and faciesassemblages. Journal of Sedimentary Research, 64: 450-489.

Chen, Z. N., Chen, F. J., Wang, Q., 2005. Types of normalfaults'soft linkage and corresponding tramsfer zones. Geoscience, 19 (4): 495-499 (in Chinese with Englishabstract).

Cherry, S. T. J., 1993. The interaction of structure and sedimentary process controlling deposition of the Upper Jurassic Brae Formation conglomerate, Block16/17, NorthSea. In: Paeker, J. R., ed., Petroleum geology of northwest Europe, Proceedings of the 4th conference. TheGeological Society, London, 4: 387-400.

Feng, Y. L., Zhou, H. M., Li, S. T., et al., 2004. Sequencetypes and subtle trap exploration in continental rift basin: A case study of Lower Tertiary of the Nanpu depression. Earth Science—Journal of China University of Geosciences, 29 (5): 603-608 (in Chinese with Eng-lish abstract).

Galloway, W. E., Hobday, D. K., 1983. Terrigenous clastic depositional systems—Applications to petroleum, coal and uraniumexploration. Springer-Verlag, New York, 423.

Gawthorpe, R. L., Colella, A., 1990. Tectonic controls oncoarse-grained delta depositional systems in rift basins. In: Colella, A., Prior, D., eds., Coarse-grained deltas. Special Publications of the International Association of Sedimentologists, 10: 113-120.

Gawthorpe, R. L., Hurst, J. M., 1993. Transfer zones in extensional basins: Their structural style and influence ondrainage development and stratigraphy. Journal of theGeological Society, London, 150 (6): 1137-1152. doi: 10.1144/gsjgs.150.6.1137

Heward, A. P., 1978. Alluvial fan sequence and megase-quence models: With examples from WestphalianD-Stephanian Bcoalfields, northern Spain. In: Miall, A. D. ed., Fluvial sedimentology. Memoir of the Canadian Society of Petroleum Geologists, 5: 669-702.

Leeder, M. R., Gawthorpe, R. L., 1987. Sedimentary modelsfor extensional tilt-block/half-graben basins. In: Cow-ard, M. P., Dewey, J. F., Hancock, P. L., eds., Conti-nental extensional tectonics. Geological Society, Lon-don, Special Publications, 28: 139-152.

Lin, C. S., Pan, Y. L., Xiao, J. X., et al., 2000. Structuralslope-break zone: Key concept for stratigraphic sequenceanalysis and petroleum forecasting in fault subsidencebasins. Earth Science—Journal of China University of Geosciences, 25 (3): 260-266 (in Chinese with Englishabstract).

Magnavita, L. P., Da Silva, H. T. F., 1995. Rift border system: The interplay between tectonics and sedimentationin the Reconcavo basin, northeastern Brazil. AAPGBulletin, 79 (11): 1590-1607.

Morley, C. K., Nelson, R. A., Patton, T. L., et al., 1990. Transfer zones in the East Africa rift systemand theirrelevance to hydrocarbon exploration in rifts. AAPGBulletin, 74 (8): 1234-1253.

Ravnas, R., Steel, R. J., 1998. Architecture of marine rift-mbasin successions. AAPG Bulletin, 82 (1): 110-146.

Roberts, S., Jackson, J., 1991. Active normal faulting in cen-tral Greece: An overview. In: Robert, A. M., Yielding, G., Freeman, B., eds., The geometry of normal faults. Geological Society, London, Special Publications, 56: 125-142.

Schlische, R. W., 1995. Geometry and origin of fault-relatedfolds in extensional settings. AAPG Bulletin, 79: 1661-1678.

Surlyk, F., 1978. Submarine fan sedimentation along faultscarps on tilted fault blocks (Jurassic-Creataceousboundary, East Greenland). Bulletin Grønlands Geolo-giske Undersøgelse, 128: 359-382.

Surlyk, F., 1984. Fan-delta to submarine fan conglomeratesof the Volgian-Valanginian Wollaston foreland group, East Greenland. In: Koster, E. H., Steel, R. J., eds., Sedimentology of gravels and conglomerates. Memoirofthe Canadian Society of Petroleum Geologists, 10: 359-382.

Surlyk, F., Noe-Nygaard, N., Dam, G., 1993. High and lowresolution sequence stratigraphy in lithological prediction—Examples fromthe Mesozoic around the northernNorth Atlantic. In: Parker, J. R., ed., Petroleum geology of northwest Europe, Proceedings of the4th conference. Geological Society, London, 199-214.

Turner, C. C., Cohen, J. M., Connell, E. R., et al., 1987. Adepositional model for the South Brae oilfield. In: Brooks, J., Glennie, K. W., eds., Petroleum geology ofnorthwest Europe. Graham and Trot man, London, 853-864.

Vail, P. R., Mitchum, R. M., Todd, R. G., et al., 1977. Seis-mic stratigraphy and global changes of sea level. In: Payton, C. E., ed., Seismic stratigraphy-applications tohydrocarbon exploration. AAPG Memoir, 26: 49-212.

Wang, L. C., Zhang, J. L., 1996. Sedimentary environmentand sedimentary facies. Prtroleum Industrry Press, Beijing, 148-149 (in Chinese).

Wang, Y. M., Liu, H., Li, L. C., et al., 2002. Types and distribution characteristics of slope breaks of large-typedown-warped lake basins. Earth Science—Journal of China University of Geosciences, 27 (6): 683-687 (inChinese with English abstract).

Wheeler, G., 1939. Triassic faultline deflections and associated warping. Journal of Geology, 47 (4): 337-370. doi: 10.1086/624784

Zhao, B., Meng, X. H., Hou, J. Q., 2007. Building and visualization of 3D seismic model. Earth Science—Journal of China University of Geosciences, 32 (4): 549-553 (in Chinese with English abstract).

陈昭年, 陈发景, 王琦, 2005. 正断层软联接及其传递带类型. 现代地质, 19 (4): 495-499. doi: 10.3969/j.issn.1000-8527.2005.04.003

冯有良, 周海民, 李思田, 等, 2004. 陆相断陷盆地层序类型与隐蔽油气藏勘探——以南堡凹陷古近系为例. 地球科学——中国地质大学学报, 29 (5): 603-608. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200405015.htm

林畅松, 潘元林, 肖建新, 等, 2000. "构造坡折带"——断陷盆地层序分析和油气预测的重要概念. 地球科学——中国地质大学学报, 25 (3): 260-266. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200003008.htm

王良忱, 张金亮, 1996. 沉积环境和沉积相. 北京: 石油工业出版社, 148-149.

王英民, 刘豪, 李立诚, 等, 2002. 准噶尔大型坳陷湖盆坡折带的类型和分布特征. 地球科学——中国地质大学学报, 27 (6): 683-687. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200206005.htm

赵博, 孟小红, 侯建全, 2007. 三维地震建模与可视化. 地球科学——中国地质大学学报, 32 (4): 549-553. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200704019.htm

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