RESEARCH PAPER

Three-dimensional discrete element numerical simulation of Paleogene salt structures in the western Kuqa foreland thrust belt

  • Jianghai LI ,
  • Yu ZHANG ,
  • Honghao WANG ,
  • Dianju WANG
Expand
  • 1. The Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences, Peking University,Beijing 100871, China
    2. Institute of Oil and Gas, Peking University, Beijing 100871, China

Received date: 2019-03-18

  Revised date: 2020-01-02

  Online published: 2020-02-19

Supported by

Supported by the China National Science and Technology Major Project(2016ZX05033002);Supported by the China National Science and Technology Major Project(2016ZX05033001)

Abstract

Taking the Paleogene salt strata in the west of Kuqa foreland thrust belt as study object, the deformation features of salt structure in the compression direction and perpendicular to the compression direction were examined to find out the control factors and formation mechanisms of the salt structures. By using the three-dimensional discrete element numerical simulation method, the formation mechanisms of typical salt structures of western Kuqa foreland thrust belt in Keshen and Dabei work areas were comprehensively analyzed. The simulation results show that the salt deformation in Keshen and Dabei work areas is of forward spread type, with deformation concentrated in the piedmont zone; the salt deformation is affected by the early uplift near the compression end, pre-existing basement faults, synsedimentary process and the initial salt depocenter; in the direction perpendicular to the compression direction, salt rocks near the compression end have strong lateral mobility with the velocity component moving towards the middle part, and the closer to the middle, the larger the velocity will be, so that salt rocks will aggregate towards the middle and deform intensely, forming complex folds and separation of salt structures from salt source, and local outcrop with thrust faults. Compared with 2D simulation, 3D simulation can analyze salt structures in the principal stress direction and direction perpendicular to the principal stress, give us a full view of the formation mechanisms of salt structures, and guide the exploration of oil and gas reservoirs related to salt structures.

Cite this article

Jianghai LI , Yu ZHANG , Honghao WANG , Dianju WANG . Three-dimensional discrete element numerical simulation of Paleogene salt structures in the western Kuqa foreland thrust belt[J]. Petroleum Exploration and Development, 2020 , 47(1) : 68 -79 . DOI: 10.1016/S1876-3804(20)60006-4

References

[1] HE Dengfa, LI Desheng, HE Jinyou , et al. Comparison in petroleum geology between Kuqa depression and Southwest depression in Tarim Basin and its exploration significance. Acta Petrolei Sinica, 2013,34(2):201-218.
[2] WANG Xin, TANG Pengcheng, XIE Huiwen , et al. Cenozoic salt structures and evolution in the western Kuqa depression, Tarim Basin, China. Geotectonina et Metallogenia, 2009,33(1):57-65.
[3] TANG Liangjie, LI Jingchang, YU Yixin , et al. Differential salt tectonic deformation and segmentation of the Kuqa foreland fold-thrust belt, Tarim Basin, northwest China. Acta Geologica Sinica, 2006,80(3):313-320.
[4] CHEN Shuping, TANG Liangjie, JIA Chengzao , et al. Salt tectonics in the western Kuqa Depression and its relation to oil and gas distribution. Acta Petrolei Sinica, 2004,25(1):30-34.
[5] LI Y, HOU G, HARI K R , et al. The model of fracture development in the faulted folds: The role of folding and faulting. Marine and Petroleum Geology, 2018,89(Part 2):243-251.
[6] YU Yixin, MA Baojun, TANG Liangjie , et al. Major factors controlling salt structures in western Kuqa Depression, Tarim Basin. Petroleum Exploration and Development, 2008,35(1):23-27.
[7] LI S, XIN W, JOHN S . Compressional salt tectonics and synkinematic strata of the western Kuqa foreland basin, southern Tian Shan, China. Basin Research, 2012,24(4):475-497.
[8] YIN Hongwei, WANG Zhe, WANG Xin , et al. Characteristics and mechanics of Cenozoic salt-Related structures in Kuqa foreland basins: Insights from physical modeling and discussion. Geological Journal of China Universities, 2011,17(2):308-317.
[9] WANG Xin, WANG Zhaoming, XIE Huiwen , et al. Cenozoic salt tectonics and physical models in the Kuqa depression of Tarim Basin China. SCIENCE CHINA Earth Science, 2010,40(12):1655-1668.
[10] LI Weibo, LI Jianghai, WANG Honghao , et al. Deformation mechanisms of Kelasu tectonic belt in Kuqa foreland thrust belt: Insight from discrete element numerical simulation. Geotectonica et Metallogenia, 2017,41(6):1001-1010.
[11] HOU Yanli, ZHANG Chuhan . Mode I-fracture simulation of concrete based on 3D distinct element method. Engineering Mechanics, 2007,24(1):37-43.
[12] GENG Y, YU H S, MCDOWELL G . Simulation of granular material behaviour using DEM. Procedia Earth & Planetary Science, 2009,1(1):598-605.
[13] WU Guanghui, WANG Zhaoming, LIU Yukui , et al. Kinematics characteristics of the Kuqa Depression in the Tarim Basin. Geological Review, 2004,50(5):476-483.
[14] TANG Pengcheng, RAO Gang, LI Shiqin , et al. The effect of salt thickness on fold lateral linkage: A case study of the anticlines in the leading edge of the western Kuqa fold and thrust belt, South Tianshan. Acta Geologica Sinica, 2018,92(3):437-448.
[15] TANG Liangjie, YU Yixin, YANG Wenjing , et al. Paleo-uplifts and salt structures and their influence on hydrocarbon accumulations in the Kuqa Depression. Acta Geologica Sinica, 2007,81(2):145-150.
[16] WANG W, YIN H, JIA D , et al. A sub-salt structural model of the Kelasu structure in the Kuqa foreland basin, northwest China. Marine & Petroleum Geology, 2017,88:115-126.
[17] LI Yanyou, QI Jiafu . Structural segmentation and mechanism in Dabei-Keshen area of Kelasu structural belt, Kuqa Depression. Chinese Journal of Geology, 2013,48(4):1177-1186.
[18] XU S, LYU X X, YUN Q S , et al. Hydrocarbon migration and accumulation history in deep reservoirs: A case study of Mesozoic sandstone gas reservoirs in the Kelasu-Yiqikelike structural belt of the Kuqa Depression, Tarim Basin. Geosciences Journal, 2019,23(1):69-86.
[19] ZHOU L, MO T, WANG Z H , et al. Classification and combination characteristics of fractures in super-deep tight sandstone reservoir of Keshen Gasfield in Tarim Basin. Natural Gas Geoscience, 2017,28(11):1668-1677.
[20] DEAN S L, MORGAN J K, FOURNIER T . Geometries of frontal fold and thrust belts: Insights from discrete element simulations. Journal of Structural Geology, 2013,53(8):43-53.
[21] GUO Y, MORGAN J K . Influence of normal stress and grain shape on granular friction: Results of discrete element simulations. Journal of Geophysical Research Solid Earth, 2004,109(B12):1-16.
[22] MORGAN J K, MCGOVERN P J . Discrete element simulations of gravitational volcanic deformation: 1. Deformation structures and geometries. Journal of Geophysical Research Solid Earth, 2005,110(B5):1-22.
[23] NAYLOR M, SINCLAIR H D, WILLETT S , et al. A discrete element model for orogenesis and accretionary wedge growth. Journal of Geophysical Research Solid Earth, 2005,110(B12):1-16.
[24] COTTON F, SCHERBAUM F, BOMMER J J , et al. Criteria for selecting and adjusting ground-motion models for specific target regions: Application to central europe and rock sites. Journal of Seismology, 2006,10(2):137-156.
[25] FUCHS S, SCHüTZ F, F?RSTER H J , et al. Evaluation of common mixing models for calculating bulk thermal conductivity of sedimentary rocks: Correction charts and new conversion equations. Geothermics, 2013,47:40-52.
[26] NIKOLINAKOU M A, HUDEC M R, FLEMINGS P B . Comparison of evolutionary and static modeling of stresses around a salt diapir. Marine & Petroleum Geology, 2014,57:537-545.
[27] FINCH E, HARDY S, GAWTHORPE R . Discrete-element modelling of extensional fault-propagation folding above rigid basement fault blocks. Journal of Structural Geology, 2003,25(4):515-528.
[28] HARDY S . Structural evolution of calderas: Insights from two-dimensional discrete element simulations. Geology, 2008,36(12):927-930.
[29] HARDY S, MCCLAY K, MU?OZ J A . Deformation and fault activity in space and time in high-resolution numerical models of doubly vergent thrust wedges. Marine & Petroleum Geology, 2009,26(2):232-248.
[30] ZHU Huanchun . PFC and application case of caving study. Chinese Journal of Rock Mechanics and Engineering, 2006,25(9):1927-1932.
[31] ZHANG Long, TANG Huiming, XIONG Chengren , et al. Movement process simulation of high-speed long-diatance Jiweishan landslide with PFC3D. Chinese Journal of Rock Mechanics and Engineering, 2012,31(S1):2601-2611.
[32] JIANG Mingjing, ZHOU Wei, LIU Jingde , et al. A constitutive model for anisotropic structured sandy soil based on micromechanical mechanism. Rock and Soil Mechanics, 2016,37(12):3347-3355.
[33] FENG J, REN Q, XU K . Quantitative prediction of fracture distribution using geomechanical method within Kuqa Depression, Tarim Basin, NW China. Journal of Petroleum Science and Engineering, 2018,162:22-34.
[34] QI Jiafu, LEI Ganglin, LI Minggang , et al. Analysis of structure model and formation mechanism of Kelasu structure zone, Kuqa Depression. Geotectonina et Metallogenia, 2009,33(1):49-56.
[35] LI Yuejun, YANG Haijun, ZHAO Yan , et al. Tectonic framework and evolution of South Tianshan, NW China. Geotectonina et Metallogenia, 2009,33(1):94-104.
[36] XU Li, LI Jianghai, WANG Honghao , et al. Paleogene sedimentary characteristics and salt lake evolution in the Dabei area, Kuqa Depression. Special Oil & Gas Reservoirs, 2016,23(5):56-61.
[37] XIAO W, WINDLEY B F, ALLEN M B , et al. Paleozoic multiple accretionary and collisional tectonics of the Chinese Tianshan orogenic collage. Gondwana Research, 2013,23(4):1316-1341.
Outlines

/