Advances on Relationship between Strike-Slip Structures and Hydrocarbon Accumulations in Large Superimposed Craton Basins, China
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摘要: 在系统回顾走滑断裂研究历史、形成机制和基本构造特征的基础上，重点讨论了我国大型克拉通叠合盆地走滑构造与油气聚集方面的最新研究进展.概括起来包括：（1）走滑断裂应力和生长机制决定了走滑断裂体系和构造样式具有“平面分区、走向分段、侧向分带、垂向分层、层内分异”特征；（2）板内走滑断裂与油气富集关系表明走滑断裂带具有“控源、控输、控储、控圈、控藏和控富”作用；（3）这种断控孔缝洞型储集体的表征可以从露头测量→测井资料刻画→三维地震雕刻3个方面进行，其核心是裂缝密度的分布与预测；（4）板内走滑断裂带断控油气藏通源性、充注过程和年代学研究为克拉通盆地深层-超深油气勘探提供了新的工具.另外，对本专辑发表的论文进行了评述.以期对推动我国克拉通盆地深层-超深层油气勘探起到抛砖引玉之功效.Abstract: On the basis of review of strike-slip fault research history, formation mechanism and principal structural characteristics, the relationship between strike-slip fault in intraplate cratonic basins and hydrocarbon accumulation in China are emphatically discussed in this paper, which can be outlined as follows.(1) Strike-slip fault stress, growth mechanism and structural style determine the strike-slip fault belt having five features of "different systems in planar, segmentation in strike, zoning in lateral, layering in vertical, and differentiation within layers". (2) The relationship between strike-slip faults within intraplate and hydrocarbon accumulation indicates that the strike-slip fault plays six roles of "controlling source, transmission, reservoir enhancement, trap-forming, reservoiring, and hydrocarbon enrichment". (3) The delineation of this strike-slip-controlled reservoir bodies can be conducted from outcrop measurement to log data depiction to 3D seismic data characterization in steps, and the key is fracture distribution acquirement and fracture density prediction. And (4) the studies of hydrocarbon sourcing, charging and dating for the exploration of strike-slip-controlled reservoirs in intraplate provides a strong tool in the deep and ultra-deep cratonic basins in china. In addition, the comments of published papers in this special issue have been made. The expectation of this issue is serving as a modest spur to promote hydrocarbon exploration to come forward with the valuable contributions in China in future.
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图 1 走滑断裂及其与油气聚集相关研究发表的论文统计直方图
统计时间为1982年1月1日至2022年10月30日；中文文献来自于中国知网CNKI；英文文献来自于Web of Science
Fig. 1. Statistical histograms of globally published articles with the topics of strike-slip fault and its related hydrocarbon accumulation
图 2 走滑断层基本几何属性图(据Aydin and Berryman, 2010)
a.沿走滑断层分段以及各段的长度（l1、l2、l3）、高度（h1、h2）、阶步数（s1、s2、s3）.阶步长度（o）和阶步宽度（或断层离距w）；b.走滑断层的内部构型包括断岩、断面和由损伤带所围的断核
Fig. 2. The basic geometric attribution of strike-slip fault (after Aydin and Berryman, 2010)
图 3 走滑断层宽度与位移关系
据Aydin and Nur（1982）；斜率显示长/宽比为l/w=3.2
Fig. 3. Plot of width of strike-slip fault vs. displacement
图 4 走滑断层厚度(T)与位移(D)关系(据Fossen，2010)
Fig. 4. Plot of thickness of strike-slip fault vs. displacement (Fossen, 2010)
图 5 运用应变椭圆图示右行力偶产生的各种走滑构造
据Harding（1974）；PDZ为主位移带；P为同向剪切断层；T为张断层；R和R’分别为同向剪切和反向断层；ϕ为内摩擦角
Fig. 5. Using strain ellipse produced by dextral couple schematically to exhibit composite structures in strike-slip fault belt
图 6 沿着走滑断层系统弯曲带或断阶带发育的双重伸展(张扭)和双重挤压(压扭)示意(据Fossen，2010)
Fig. 6. Schematic diagram showing contractional extensional strike-slip duplexes (transtensional deformation) and strike-slip duplexes (transpressional deformation) at bends or stepover along strike-slip fault system (Fossen, 2010)
图 7 走滑断裂带中不同尺度下雁列方解石脉显示的剪切构造照片
a.塔里木盆地跃进3-3井奥陶系一间房组(7 187.35 m)走滑断裂带内垂直雁列方解石脉岩心照片；b.塔里木盆地富满油田满深5井奥陶系(7 608.12 m)走滑断裂带内亮晶砂屑灰岩中雁列状微裂缝(蓝色铸体薄片所示)显微照片(张秋艳提供)
Fig. 7. Photos of the en echelon calcite veins showing shearing structures in the strike-slip fault belts
图 8 塔里木盆地顺托果勒地区FⅠ17号走滑断裂带复式花状构造(引自能源，2021，内部材料
Fig. 8. 3D seismic profile showing composite flower structures in No. FⅠ17 strike-slip fault in Shuntuoguole area, Tarim basin (after Neng, 2021)
图 9 塔里木盆地台盆区加里东中期Ⅲ幕应力场与走滑断裂带体系划分叠合(据李国会等，2021修改)
Fig. 9. Map showing the strike-slip fault system division in the cratonic Tarim basin (modified from Li et al., 2021)
图 10 走滑断层损伤带立体概念模型图(a)和确定断层损伤带及断核宽度示意(b)(据Choi et al., 2016修改)
Fig. 10. Conceptual block diagram of strike-slip fault damage zone (a) and schematic diagram of determining the fault damage zone width (b) (after Choi et al., 2016)
图 11 走滑断层不同生长阶段损伤带演化概念模型(de Joussineau and Aydin, 2007)
Fig. 11. Conceptual model of damage zone of strike-slip fault during different growth stages (de Joussineau and Aydin, 2007)
图 12 考虑不同因素的损伤带构造样式概念模型(de Joussineau and Aydin, 2007)
Fig. 12. Conceptual models of structural pattern of damage zone under the considering of different factors (de Joussineau and Aydin, 2007)
图 13 走滑断层损伤带类型划分图(据Peacock et al., 2017修改)
Fig. 13. Diagram showing classification of different types of strike-slip fault damage zones (modified from Peacock et al., 2017)
图 14 走滑断裂带断控洞穴(a)和溶洞(b)
a.塔里木盆地富满油田满深4井(FⅠ17走滑断裂带上)FMI成像测井显示的近10 m的洞穴(据王清华等，2022中图2)；b.鄂尔多斯盆地南缘泾河油田永和走滑断裂带上JH9井长811砂岩中发育的溶蚀孔洞
Fig. 14. The cave (a) and vugs (b) genetically controlled by strike-slip faults
图 15 运用常规测井曲线预测裂缝带流程图
Fig. 15. The flow chart of using traditional log curves to predict fracture zones
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