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Styles of Salt Tectonics in the Sab'atayn Basin, Onshore Yemen

机译:Sab'atayn盆地的盐构造型风格,陆上也门

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In the Sab'atayn Basin of Yemen hydrocarbons were generated from pre-salt Upper Jurassic source rocks during the Cenozoic and the salt provides the ultimate seal for the pre-salt and intra-salt traps. Therefore the proper understanding of salt tectonics is critical for ongoing hydrocarbon exploration efforts in the Sab'atayn Basin. A variety of distinct salt tectonic features are present in the Sab'atayn Basin. Based on the regional interpretation of 2D seismic and locally available 3D seismic reflection data calibrated by exploration wells in the central part of the basin, an Upper Jurassic evaporite formation ("salt" from this point on) produced numerous salt rollers, pillows, reactive, flip-flop, active and falling diapirs. Due to regional extension, halokinetics began by formation of salt rollers, as soon as the early Cretaceous, within just a few million years after the deposition of the Tithonian Sab'atayn Formation. The salt locally formed salt pillows which evolved to salt diapirs and diapiric salt walls as the result of renewed extension in the basin. As the result of a prominent extensional episode at the end of the Cretaceous most of the diapiric walls in the basin are controlled by large normal faults on their updip flanks. Some of the diapiric walls even evolved into falling diapirs due to ongoing extension. As the post-Cretaceous sedimentary cover is largely missing in the study area, the assumed reactivation of salt structures during the Cenozoic remains poorly constrained. As the Sab'atayn Formation has typically several massive salt intervals in it, it defines post-, intra- and pre-salt play types in the basin. However, other than just providing traps and seals in the basin, salt tectonics is also very important for source rock maturation in the basin. As there are many salt diapirs in the study area, their cooling effect on the the pre-salt hydrocarbon kitchens appears to be quite significant, based on our preliminary basin modelling efforts.
机译:在新生代期间从盐前侏罗纪源岩生成了也门烃的Sab'atayn盆地,盐为预盐和盐陷阱提供了最终密封。因此,对盐构构的正确理解对于持续的Sab'atayn盆地的持续碳氢化合物勘探工作至关重要。 Sab'atayn盆地中存在各种不同的盐构造特征。根据盆地中部部分勘探井校准的2D地震和本地可用的3D地震反射数据的区域解释,侏罗纪蒸发产物(“盐”从这一点)产生了许多盐辊,枕头,反应性,触发器,活跃和落后的催泪。由于区域延期,脊柱管术开始形成盐辊,一旦初期白垩纪,在沉积Tithonian Sab'atayn形成后就在几百万年内。由于盆内的重新延伸,盐局部形成的盐枕头在盐酸尿布和酸性盐壁上发展。由于在盆中的大部分白垩纪的末端末端突出的突出剧集的结果受到腹部腹部侧翼的大型正常断层的控制。由于持续的延伸,一些涂抹墙甚至进化成落后落叶。随着在研究领域的后白垩纪沉积覆盖在很大程度上缺失,新生代期间盐结构的假定再活化仍然受到严重的限制。由于Sab'atayn形成通常有几种大量的盐间隔,它定义了盆中的后,内部和盐前的戏剧类型。然而,除了仅在盆地中提供陷阱和密封外,盐构造术对盆地的来源岩石成熟也非常重要。由于研究领域存在许多盐尿布,因此它们对盐前碳氢化合物厨房的冷却效果似乎非常重要,基于我们的初步盆地建模努力。

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