Oil & Gas Geology ›› 2024, Vol. 45 ›› Issue (5): 1226-1246.doi: 10.11743/ogg20240503
• Petroleum Geology • Previous Articles Next Articles
Juncheng QIAO1,2(), Shaoying CHANG1,3, Jianhui ZENG1,2(), Peng CAO3, Keliang DONG1,2, Mengxiu WANG3, Jining YANG1,2, Yazhou LIU1,2, Hui LONG1,2, Ting AN4, Rui YANG5, Lin WEN1,2
Received:
2024-05-22
Revised:
2024-09-12
Online:
2024-10-30
Published:
2024-11-06
Contact:
Jianhui ZENG
E-mail:Juncheng.Qiao@cup.edu.cn;zengjh@cup.edu.cn
CLC Number:
Juncheng QIAO, Shaoying CHANG, Jianhui ZENG, Peng CAO, Keliang DONG, Mengxiu WANG, Jining YANG, Yazhou LIU, Hui LONG, Ting AN, Rui YANG, Lin WEN. Origin of differential hydrocarbon accumulation in ultra-deep carbonate reservoirs along strike-slip fault zones in the Fuman area, northern Tarim Basin[J]. Oil & Gas Geology, 2024, 45(5): 1226-1246.
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Table 1
Characteristics of the connection to source rocks and hydrocarbon transport capacity of strike-slip fault zones in the Fuman area"
通源性 | 输导性 | ||||||||
---|---|---|---|---|---|---|---|---|---|
类型 | 模式图 | 断裂附近地层变形特征 | 变形强度 | 类型 | 模式图 | 断裂带附近地层变形特征 | 变形强度 | ||
强通源型 | 直接错断强通源型 | 地层直接错断,断距明显,地层平直,破碎程度高 | >0.10 | 强输导型 | 直接错断强输导型 | 膏岩层直接错断,断距明显,地层平直,破碎程度较高 | >0.15 | ||
未错断强通源型 | 地层未发生明显错断,地层弯曲变形程度大,地层破碎程度高 | >0.10 | 未错断强输导型 | 膏岩层未发生明显错断,地层弯曲变形程度大,地层破碎程度高 | >0.09 | ||||
未错断中通源型 | 地层未发生明显错断,地层弯曲变形程度幅度较大,地层破碎程度较高 | 0.06~0.10 | 未错断中输导型 | 膏岩层未发生明显错断,地层弯曲变形程度幅度较大,地层破碎程度较高 | 0.05~0.09 | ||||
未错断弱通源型 | 地层未发生明显错断,地层完全变形程度低,较平直,地层破碎程度较低 | 0.02~0.06 | 未错断弱输导型 | 膏岩层未发生明显错断,地层完全变形程度低,较平直,地层破碎程度较低 | <0.09 | ||||
极弱通源型 | 断层未断至烃源岩层 | 无 | 无 | 无 | 无 | 无 |
Table 2
Evaluation of the storage capacity of carbonate reservoirs in the Ordovician Yijianfang Formation, Fuman area"
储集性能 | 优储集 | 中储集 | 差储集 |
---|---|---|---|
储集模式 示意图 | |||
储集系数 | >1.5 | 0.5~1.5 | <0.5 |
储集空间类型 | 分支断裂发育,断裂面附近发育规模性的洞穴,向周缘发育宽度较大的缝洞发育带和衍生裂缝带,洞穴和孔洞是主要储集空间 | 分支断裂较发育,仅在主干断裂面附近发育较小规模的洞穴,周缘缝洞发育带规模减小,发育较大规模的衍生裂缝带,洞穴、孔洞和裂缝是主要储集空间 | 分支断裂不发育,洞穴不发育,周缘缝洞发育带规模较小,发育较大规模的衍生裂缝带,孔洞、裂缝及基质孔隙是主要储集空间 |
储集空间形态 | 球形、纺锤形、条形 | 以球形为主 | 以条形或者纺锤形为主 |
储集物性特征 | |||
微观储集空间特征 | |||
发育应力段 | 拉分段为主,挤压段次之 | 挤压段为主,平移段次之 | 主要出现在平移段,少量出现在挤压段 |
Table 3
Pearson correlations between parameters for hydrocarbon migration and accumulation and the degree of hydrocarbon enrichment in strike-slip fault zones in the Fuman area"
成藏运聚条件参数 | 折日产油气当量 | 累计产油 | 累计产气 | 累计产油气当量 | |
---|---|---|---|---|---|
源岩变形强度 | 皮尔逊相关系数 | 0.274 | 0.621** | 0.732** | 0.667** |
显著性水平(双尾) | 0.304 | 0.008 | 0.001 | 0.003 | |
源岩断距/m | 皮尔逊相关系数 | 0.068 | 0.143 | 0.136 | 0.144 |
显著性水平(双尾) | 0.803 | 0.583 | 0.604 | 0.582 | |
膏盐岩变形强度 | 皮尔逊相关系数 | 0.418* | 0.183 | 0.354 | 0.231 |
显著性水平(双尾) | 0.042 | 0.380 | 0.082 | 0.266 | |
膏盐岩断距/m | 皮尔逊相关系数 | 0.507* | 0.299 | 0.516** | 0.361 |
显著性水平(双尾) | 0.012 | 0.147 | 0.008 | 0.076 | |
膏盐岩厚度/m | 皮尔逊相关系数 | 0.767** | 0.044 | 0.219 | 0.091 |
显著性水平(双尾) | 0 | 0.834 | 0.292 | 0.666 | |
储集系数 | 皮尔逊相关系数 | 0.355 | 0.262 | 0.300 | 0.277 |
显著性水平(双尾) | 0.125 | 0.251 | 0.187 | 0.224 |
Table 4
Characteristic values and variance percentages of six principal components of the hydrocarbon migration and accumulation parameters in strike-slip fault zones in the Fuman area"
主成分编号 | 初始特征值 | 方差百分比/% | 累积百分比/% |
---|---|---|---|
1 | 3.682 | 61.364 | 61.364 |
2 | 1.084 | 18.070 | 79.434 |
3 | 0.546 | 9.103 | 88.537 |
4 | 0.500 | 8.327 | 96.864 |
5 | 0.127 | 2.119 | 98.983 |
6 | 0.061 | 1.017 | 100.000 |
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