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Structural characteristics and petroleum exploration of Levant Basin in Eastern Mediterranean

机译:东地中海黎凡特盆地的构造特征和石油勘探

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By using geologic and seismic data, this study restored the proto-type basins and lithofacies paleogeography of the Levant basin in Eastern Mediterranean during main geological periods, carried out comparison analysis on the basin architecture characteristics, and based on careful examination of the characteristics of discovered gas reservoirs, established the reservoir forming pattern and discussed the favorable reservoir forming combinations and future exploration direction in this region. Three structural architectures can be identified in the basin, the early-stage faults, the mid-stage faults and the late-stage faults. The early-stage faults are mainly controlled by intercontinental depression, which were less influenced by later compression stress in the southern deep water area of the basin. Controlled by the lateral structural stress and the Syrian Arc Fold Belt, the mid-stage faults became less active from north to south and from east to west. Influenced by the collision and/or Dead Sea strike-slip Fault Zone, the late-stage faults were active but did not pierce the thick Upper Miocene evaporites. Combined with the discovered reservoirs and outcrops, the Mesozoic sandstones and carbonates in deep water area near Eratosthenes seamount of Israel offshore and the Cenozoic carbonates and Tamar sands of Lebanon offshore are the main petroleum exploration targets in the next step.
机译:利用地质和地震数据,本研究恢复了地中海东部主要地质时期黎凡特盆地的原型盆地和岩相古地理,对盆地构造特征进行了比较分析,并在仔细检查发现的特征的基础上进行了研究。气藏,建立了成藏模式,并讨论了该地区有利的成藏组合和未来的勘探方向。盆地中可识别出三种构造体系,即早期断裂,中期断裂和晚期断裂。早期断层主要受洲际depression陷控制,盆地南部深水区的后期压缩应力影响较小。在横向结构应力和叙利亚弧形褶皱带的控制下,中段断裂从北向南和从东向西的活动性减弱。受碰撞和/或死海走滑断层带的影响,晚期断层活跃,但没有刺穿厚的中新世蒸发岩。结合已发现的储层和露头,以色列近海埃拉托塞内斯海山附近深水区的中生代砂岩和碳酸盐以及黎巴嫩近海的新生代碳酸盐岩和塔玛尔砂岩是下一步的主要石油勘探目标。

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