油气勘探

砂体融合的定量表征及其对储集层连通性的控制

  • 张磊夫 ,
  • 王红亮 ,
  • 李英烈 ,
  • 潘懋
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  • 1. 北京大学地球与空间科学学院,北京 100871;
    2. 中国地质大学(北京)能源学院,北京 100083;
    3. 中国地质调查局油气资源调查中心,北京 100029
张磊夫(1987-),男,湖南湘潭人,北京大学地球与空间科学学院在站博士后,主要从事沉积学与储集层建模方面的研究工作。地址:北京市海淀区颐和园路5号,北京大学地球与空间科学学院,邮政编码:100871。E-mail:leifu.zhang@pku.edu.cn

收稿日期: 2016-03-30

  修回日期: 2016-12-30

  网络出版日期: 2017-05-22

基金资助

中国博士后科学基金(2016M591016)

Quantitative characterization of sandstone amalgamation and its impact on reservoir connectivity

  • ZHANG Leifu ,
  • WANG Hongliang ,
  • LI Yinglie ,
  • PAN Mao
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  • 1. School of Earth and Space Sciences, Peking University, Beijing 100871, China;
    2. School of Energy Resources, China University of Geosciences, Beijing 100083, China;
    3. Oil and Gas Survey, China Geological Survey, Beijing 100029, China

Received date: 2016-03-30

  Revised date: 2016-12-30

  Online published: 2017-05-22

摘要

以浊积朵叶体沉积为例,介绍了砂体融合现象的类型与形成原因,讨论了砂体融合现象对沉积环境及砂体叠置样式的指示作用,并应用砂体融合比定量描述了砂体之间相互融合的程度。在以砂泥为主的碎屑沉积中,砂体之间的相互融合非常普遍,其包括砂体对泥质隔夹层的侵蚀并与其他砂体融合两个方面。对已有文献的统计分析表明,砂体融合比在不同的构型层次有显著差异,在此基础上,用基于目标的建模方法建立了3组砂地比、单砂层尺寸相同但具有不同层次与不同砂体融合比的朵叶体三维模型。对模型的连通性分析表明:模型引入的沉积层次越多,连通性越差;对沉积层次一致的模型而言,砂体融合比越高,连通性越好。图8表2参35

本文引用格式

张磊夫 , 王红亮 , 李英烈 , 潘懋 . 砂体融合的定量表征及其对储集层连通性的控制[J]. 石油勘探与开发, 2017 , 44(2) : 205 -212 . DOI: 10.11698/PED.2017.02.04

Abstract

Taking turbidity lobe deposits as an example, the types and formation mechanisms of sandstone amalgamation were discussed, the indications of sandstone amalgamations to sedimentary environment and stacking pattern of sand bodies were investigated, and “amalgamation ratio” was employed to quantitatively describe the degree of sandstone amalgamation. Sandstone amalgamation is a common sedimentological phenomenon in sand/mud dominated clastic deposits, which generally consists of two processes: erosion of inter-sand mudstone barriers and amalgamation of sandstone beds which were previously separated by the mudstone barriers. Statistics analysis suggests that amalgamation ratio varies greatly in different hierarchical levels of structures. Based on these analyses, three sets of conceptual lobe 3D models with identical NTG (net to gross ratio) and bed sizes but different hierarchies and different amalgamation ratio using an object-based modeling approach. Static connectivity analysis of these models suggests that the more the hierarchical levels, the worse connectivity the model has; for models with identical hierarchical settings, the higher the amalgamation ratio, the better the connectivity.

参考文献

[1] WALKER R G. Shale grit and Grindslow shales: Transition from turbidite to shallow water sediments in the upper Carboniferous of northern England[J]. Journal of Sedimentary Research, 1966(1): 90-114.
[2] MUTTI E, RICCI LUCCHI F. Turbidites of the northern Apennines: Introduction to facies analysis[J]. International Geology Review, 1978, 20(2): 125-166.
[3] BOUMA A H. Introduction to submarine fans and related turbidite systems: Submarine fans and related turbidite systems[M]. New York: Springer, 1985: 3-5.
[4] CHAPIN M, DAVIES P, GIBSON J, et al. Reservoir architecture of turbidite sheet sandstones in laterally extensive outcrops, Ross Formation, western Ireland: Submarine fans and turbidite systems[M]. New York: Springer, 1994: 53-68.
[5] ROMANS B W, HUBBARD S M, GRAHAM S A. Stratigraphic evolution of an outcropping continental slope system, Tres Pasos Formation at Cerro Divisadero, Chile[J]. Sedimentology, 2009, 56(3): 737-764.
[6] GRUNDVÅG S A, JOHANNESSEN E P, HELLAND-HANSEN W, et al. Depositional architecture and evolution of progradationally stacked lobe complexes in the Eocene Central Basin of Spitsbergen[J]. Sedimentology, 2014, 61(2): 535-569.
[7] MATTERN F. Amalgamation surfaces, bed thicknesses, and dish structures in sand-rich submarine fans: Numeric differences in channelized and unchannelized deposits and their diagnostic value[J]. Sedimentary Geology, 2002, 150(3): 203-228.
[8] MACDONALD H A, PEAKALL J, WIGNALL P B, et al. Sedimentation in deep-sea lobe-elements: Implications for the origin of thickening-upward sequences[J]. Journal of the Geological Society, 2011, 168(2): 319-332.
[9] STEPHEN K D. Outcrop-based stochastic modelling of turbidite amalgamation and its effects on hydrocarbon recovery[J]. Petroleum Geoscience, 2001, 7(2): 163-172.
[10] MANZOCCHI T, WALSH J J, TOMASSO M, et al. Static and dynamic connectivity in bed-scale models of faulted and unfaulted turbidites[J]. Geological Society London Special Publications, 2007, 292(1): 309-336.
[11] ELLIOTT T. Megaflute erosion surfaces and the initiation of turbidite channels[J]. Geology, 2000, 28(2): 119-122.
[12] ZHANG Leifu, MANZOCCHI T, PONTÉN A. Hierarchical parameterization and modelling of deep-water lobes[R]. Biarritz: Petroleum Geostatistics Extended Abstract, 2015.
[13] JEGOU I, SAVOYE B, PIRMEZ C, et al. Channel-mouth lobe complex of the recent Amazon fan: The missing piece[J]. Marine Geology, 2008, 252(1): 62-77.
[14] PRÉLAT A, HODGSON D M, FLINT S S. Evolution, architecture and hierarchy of distributary deep-water deposits: A high-resolution outcrop investigation from the Permian Karoo Basin, South Africa[J]. Sedimentology, 2009, 56(7): 2132-2154.
[15] STRAUB K M, PYLES D R. Quantifying the hierarchical organization of compensation in submarine fans using surface statistics[J]. Journal of Sedimentary Research, 2012, 82(11): 889-898.
[16] BERNHARDT A, JOBE Z R, LOWE D R. Stratigraphic evolution of a submarine channel-lobe complex system in a narrow fairway within the Magallanes foreland basin, Cerro Toro Formation, southern Chile[J]. Marine & Petroleum Geology, 2011, 28(3): 785-806.
[17] DUTTON S P, FLANDERS W A, BARTON M D. Reservoir characterization of a Permian deep-water sandstone, East Ford field, Delaware basin, Texas[J]. AAPG Bulletin, 2003, 87(4): 609-627.
[18] DRINKWATER N J, PICKERING K T. Architectural elements in a high-continuity sand-prone turbidite system, Late Precambrian Kongsfjord Formation, Northern Norway: Application to hydrocarbon reservoir characterization[J]. AAPG Bulletin, 2001, 85(10): 1731-1757.
[19] PYLES D R, STRACHAN L J, JENNETTE D C. Lateral juxtapositions of channel and lobe elements in distributive submarine fans: Three-dimensional outcrop study of the Ross Sandstone and geometric model[J]. Geosphere, 2014, 10(6): 1104-1122.
[20] JOHNSON S D, FLINT S, HINDS D, et al. Anatomy, geometry and sequence stratigraphy of basin floor to slope turbidite systems, Tanqua Karoo, South Africa[J]. Sedimentology, 2001, 48(5): 987-1023.
[21] SULLIVAN M D, FOREMAN J L, STERN D, et al. An integrated approach to characterization and modeling of deep-water reservoirs, Diana field, Western Gulf of Mexico[C]//Integration of outcrop and modern analogs in reservoir modeling. Houston: AAPG Memoir 80, 2004: 215-234.
[22] HODGSON D M, FLINT S S, HODGETTS D, et al. Stratigraphic evolution of fine-grained submarine fan systems, Tanqua Depocenter, Karoo Basin, South Africa[J]. Journal of Sedimentary Research, 2006, 76(1): 20-40.
[23] ZHANG Leifu, MANZOCCHI T, HAUGHTON P D W. Impact of sedimentological hierarchy on sandstone connectivity in deep-water lobes-an object-based modelling approach[R]. London: 75 th EAGE Conference & Exhibition Incorporating SPE EUROPEC, 2013.
[24] LARUE D K, HOVADIK J M. Connectivity of channelized reservoirs: A modelling approach[J]. Petroleum Geoscience, 2006, 12(4): 291-308.
[25] HOVADIK J M, LARUE D K. Static characterizations of reservoirs: Refining the concepts of connectivity and continuity[J]. Petroleum Geoscience, 2007, 13(3): 195-211.
[26] MIALL A D. Reservoir heterogeneities in fluvial sandstones: Lessons from outcrop studies[J]. AAPG Bulletin, 1988, 72(6): 682-697.
[27] 张昌民. 储层研究中的层次分析法[J]. 石油与天然气地质, 1992, 13(3): 344-350.
ZHANG Changmin. Hierarchy analysis in reservoir researches[J]. Oil & Gas Geology, 1992, 13(3): 344-350.
[28] MIALL A D, JONES B G. Fluvial architecture of the Hawkesbury sandstone (Triassic), near Sydney, Australia[J]. Journal of Sedimentary Research, 2003, 73(4): 531-545.
[29] MAYALL M, JONES E, CASEY M. Turbidite channel reservoirs: Key elements in facies prediction and effective development[J]. Marine & Petroleum Geology, 2006, 23(8): 821-841.
[30] 邓宏文, 王红亮, 阎伟鹏, 等. 河流相层序地层构成模式探讨[J]. 沉积学报, 2004, 22(3): 373-379.
DENG Hongwen, WANG Hongliang, YAN Weipeng, et al. Architecture model of sequence stratigraphy in fluvial facies[J]. Acta Sedimentologica Sinica, 2004, 22(3): 373-379.
[31] BARTON M, O’BYRNE C J, PIRMEZ C, et al. Turbidite channel architecture: Recognizing and quantifying the distribution of channel base drapes using core and dipmeter data[R]. Houston: AAPG Annual Convention, 2010: 195-210.
[32] 林煜, 吴胜和, 王星, 等. 深水浊积朵叶储层构型模式研究[J]. 天然气地球科学, 2014, 25(8): 1197-1204.
LIN Yu, WU Shenghe, WANG Xing, et al. Research on reservoir architecture models of deep-water turbidite lobes[J]. Natural Gas Geoscience, 2014, 25(8): 1197-1204.
[33] 吴胜和, 岳大力, 刘建民, 等. 地下古河道储层构型的层次建模研究[J]. 中国科学: 地球科学, 2008, 38(S1): 111-124.
WU Shenghe, YUE Dali, LIU Jianmin, et al. Hierarchy modeling of subsurface palaeochannel reservoir architecture[J]. SCIENCE CHINA Earth Sciences, 2008, 51(2): 126-137.
[34] 岳大力, 吴胜和, 刘建民. 曲流河点坝地下储层构型精细解剖方法[J]. 石油学报, 2007, 28(4): 99-103.
YUE Dali, WU Shenghe, LIU Jianmin. An accurate method for anatomizing architecture of subsurface reservoir in point bar of meandering river[J]. Acta Petrolei Sinica, 2007, 28(4): 99-103.
[35] PAN Mao, LI Zhaoliang, GAO Zhongbo, et al. 3-D geological modeling: Concept, methods and key techniques[J]. Acta Geologica Sinica, 2012, 86(4): 1031-1036.
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