石油与天然气地质 ›› 2022, Vol. 43 ›› Issue (6): 1382-1396.doi: 10.11743/ogg20220609
杨桂林1,2(), 任战利1,2, 何发岐3, 张园园4, 王宝江5, 祁凯1,2
收稿日期:
2022-05-19
修回日期:
2022-09-24
出版日期:
2022-11-21
发布日期:
2022-11-21
第一作者简介:
杨桂林(1992—),男,博士研究生,构造断裂解释、储层沉积学与油气田开发。E?mail:基金项目:
Guilin Yang1,2(), Zhanli Ren1,2, Faqi He3, Yuanyuan Zhang4, Baojiang Wang5, Kai Qi1,2
Received:
2022-05-19
Revised:
2022-09-24
Online:
2022-11-21
Published:
2022-11-21
摘要:
断裂、裂缝对油气成藏有重要控制作用,镇泾区块位于鄂尔多斯盆地西南部不同构造单元交汇部位,受周缘强烈构造运动影响,断裂、裂缝普遍发育。在三维地震资料全覆盖的镇泾区块断裂、裂缝精细解释的基础上,对镇泾地区由断裂、伴生脆性破碎带及被其改造过的致密低渗砂岩共同构成的储集体——“断缝体”组合样式、形成期次、断缝体特征等分别进行了深入研究。断缝体主要发育5种构造组合样式,剖面上构造样式有堑垒式、阶梯式、地堑式、花状和紧闭平移式,分别对应于平面上的帚状、雁列式、平行直线式、拉分地堑式和直线式,不同组合样式具有不同的应力背景。通过地震解释和C-O同位素分析技术认为研究区断缝体带内主要存在3期断裂构造:印支期、燕山期和喜马拉雅期。其中燕山期是最主要也是最关键的断缝形成期,喜马拉雅期和印支期断裂活动相对较弱。利用K-Ar同位素、包裹体测温及热演化史分析等手段,明确了研究区三叠系延长组8段(长8段)断缝体油藏的成藏期为早白垩世中晚期。在断缝体三维刻画的基础上,结合断缝形成期与油气成藏的空间配置关系,对研究区长8段不同组合样式控藏机制进行了分析。研究结果表明雁列-阶梯式组合样式最有利于油气富集,其次是拉分地堑-花状、帚状-堑垒式组合样式,平行直线-地堑式和直线-紧闭平移式组合样式中油气富集程度最差。
中图分类号:
表1
鄂尔多斯盆地镇泾地区裂缝充填同位素分析"
井号/剖面 | 层位 | 样品深度/m | 充填物 | δ18O/‰ | δ13C/‰ | 计算温度/℃ | 计算埋深/m | 备注 |
---|---|---|---|---|---|---|---|---|
HH26 | 长6段 | 1 891.11 | 方解石 | -16.96 | -17.47 | 104.48 | 1 536.09 | |
HH198 | 延安组 | 1 813.45 | 方解石 | -15.77 | -18.77 | 87.25 | 1 222.71 | |
HH112 | 长8段 | 2 123.97 | 方解石 | -17.75 | -12.94 | 116.95 | 1 762.73 | |
HH149 | 长8段 | 2 357.11 | 方解石 | -19.08 | -6.51 | 140.00 | 2 181.85 | |
HH149 | 长8段 | 2 356.20 | 方解石 | -19.45 | -6.38 | 146.84 | 2 306.23 | |
HH152 | 延安组 | 1 748.04 | 方解石 | -20.80 | -7.40 | 173.49 | 2 790.69 | |
HH152 | 延安组 | 1 757.15 | 方解石 | -19.40 | -9.00 | 145.92 | 2 289.49 | |
HH157 | 长8段 | 2 042.28 | 方解石 | -21.60 | -4.50 | 190.47 | 3 099.49 | |
HH166 | 长8段 | 2 395.52 | 方解石 | -19.01 | -6.46 | 138.74 | 2 158.88 | |
HH166 | 长8段 | 2 389.86 | 方解石 | -20.17 | -6.66 | 160.80 | 2 560.06 | |
HH166 | 长8段 | 2 398.95 | 方解石 | -21.76 | -4.79 | 193.88 | 3 161.41 | |
HH188 | 长8段 | 2 413.25 | 方解石 | -20.85 | -9.12 | 174.50 | 2 809.09 | |
HH188 | 长8段 | 2 418.35 | 方解石 | -20.23 | -8.83 | 161.80 | 2 578.26 | |
HH192 | 长8段 | 2 462.16 | 方解石 | -20.94 | -4.27 | 176.33 | 2 842.32 | |
HH193 | 长8段 | 2 298.83 | 方解石 | -20.05 | -7.50 | 158.40 | 2 516.39 | |
HH197 | 长8段 | 2 398.27 | 方解石 | -18.98 | -6.70 | 138.19 | 2 148.90 | |
HH198 | 长8段 | 2 245.56 | 方解石 | -20.65 | -5.06 | 170.33 | 2 733.26 | |
JH36 | 长8段 | 1 376.08 | 方解石 | -23.43 | -9.15 | 232.60 | 3 865.41 | |
HH112 | 长8段 | 2 122.62 | 方解石 | -21.18 | -8.87 | 181.39 | 2 934.28 | |
HH26 | 长8段 | 2 134.57 | 方解石 | -19.70 | -1.97 | 151.60 | 2 392.69 | 原始C-O值据刘岩(2013)[ |
HH26 | 长8段 | 2 064.51 | 方解石 | -17.82 | -0.25 | 118.11 | 1 783.78 | |
HH30 | 长8段 | 2 283.28 | 方解石 | -18.66 | -1.13 | 132.46 | 2 044.73 | |
HH6 | 长8段 | 1 779.08 | 方解石 | -19.58 | -0.42 | 149.31 | 2 351.14 | |
HH105 | 长8段 | 2 264.42 | 方解石 | -18.07 | -5.77 | 122.28 | 1 859.56 | |
HH105 | 长8段 | 2 264.42 | 石英 | -18.08 | -6.26 | 122.44 | 1 862.63 | |
HH41 | 长8段 | 2 116.17 | 方解石 | -19.00 | -2.83 | 138.55 | 2 155.46 | |
汭水河剖面 | 长8段 | 野外露头 | 方解石 | -8.38 | -7.91 | 24.75 | 86.29 | |
汭水河剖面 | 长8段 | 野外露头 | 方解石 | -11.12 | -10.32 | 38.99 | 345.35 | |
HH26 | 长8段 | 2 110.20 | 方解石 | -11.36 | -0.42 | 40.74 | 377.14 | |
ZJ25 | 长8段 | 2 259.58 | 方解石 | -11.36 | 1.16 | 40.74 | 377.14 |
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