塔里木盆地富满油田走滑断裂带通源性评价
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张艳秋, 陈红汉, 王燮培, 王彭, 苏丹梅, 谢舟
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Assessment of connectivity between source rocks and strike-slip fault zone in the Fuman oilfield， Tarim Basin
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Yanqiu ZHANG, Honghan CHEN, Xiepei WANG, Peng WANG, Danmei SU, Zhou XIE
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表4 根据完全塑性介质-应力上升函数模型计算的FⅠ17走滑断裂各段通源深度参数
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Table 4 Parameters used to calculate the depths of source rocks in connection with various segments of the FⅠ17 strike-slip fault zone based on the perfectly plastic medium-stress ascending function model
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| 断裂分段 | 雁列断裂长度（L）/km | 雁列断裂深度（h）/km | 雁列角（ω）/rad | 雁列距离（S′）/km | 雁列断裂平均间隔（S）/km |
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| 范围 | 平均值 | 范围 | 平均值 | 范围 | 平均值 | 范围 | 平均值 | S=S′ sinω |
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| A段 | 4.367 3 | 3.952 5 | 2.176 3 | 2.537 3 | 0.574 1 | 0.628 7 | 1.417 9 | 1.267 8 | 0.745 6 | | 3.712 2 | 2.676 0 | 0.661 1 | 0.813 6 | | 3.852 8 | 2.745 8 | 0.611 1 | 1.352 1 | | 4.780 1 | 2.609 7 | 0.648 4 | 0.391 0 | | 4.424 2 | 2.535 5 | 0.658 0 | 1.358 1 | | 2.578 5 | 2.588 8 | 0.619 3 | 1.274 3 | | B段 | 2.405 0 | 2.475 6 | 2.002 9 | 2.102 0 | 0.946 9 | 0.935 0 | 0.320 1 | 0.280 6 | 0.225 8 | | 3.227 6 | 2.154 2 | 0.963 1 | 0.281 2 | | 2.485 7 | 2.237 5 | 0.967 6 | 0.251 3 | | 1.893 5 | 2.013 3 | 0.935 4 | 0.251 3 | | 2.366 1 | — | — | 0.862 1 | 0.299 1 | | C段 | 3.197 7 | 3.794 2 | 2.018 1 | 2.074 0 | 0.832 6 | 0.822 3 | 0.356 0 | 0.441 6 | 0.323 5 | | 3.724 2 | 2.166 2 | 0.825 5 | 0.499 6 | | 4.005 4 | 2.203 2 | 0.844 8 | 0.362 0 | | 4.056 2 | 1.908 5 | 0.817 6 | 0.559 4 | | 3.984 2 | — | — | 0.790 9 | 0.430 8 | | D段 | 3.901 1 | 4.181 6 | 3.581 9 | 3.932 6 | 0.966 9 | 0.868 6 | 1.423 9 | 1.605 4 | 1.225 5 | | 3.827 8 | 3.761 3 | 0.870 5 | 1.758 9 | | 4.816 0 | 4.454 5 | 0.768 3 | 1.633 3 |
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