中东陆上大油田高质量三维地震研究中新世水道几何形状

R. T. El-Awawdeh, A. Jarah, Sk. Arif Ahmed
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引用次数: 0

摘要

在浅层钻井灾害地震填图过程中,将几个中新世河道的几何形状解释为Langhian - Serravallian形成的海侵和高地体系域。从东北向西南方向的河道地质模式表明,它们形成于中新世伊拉克南部不稳定陆架构造背景下,在与扎格罗斯碰撞带相邻的广阔浅海前陆盆地中形成海侵-海退序列。沉积环境为开阔海相-潮上陆相-河流三角洲-暴露环境。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Miocene Channel Geometries from High Quality 3D Seismic Onshore Giant Oil Field in Middle East
During shallow drilling hazards seismic mapping campaign, several Miocene age channel geometries were interpreted as transgressive and high stand systems tracts formed from Langhian to Serravallian. Channel geologic pattern from north-east to south-west direction, suggests they were formed along unstable shelf tectonic setting of southern Iraq during Miocene, where transgressive-regressive sequence in a broad shallow foreland basin adjacent to the Zagros-collision belt. Depositional environment ranged from open-marine to supratidal and continental sabkha, fluvial-deltaic and exposure.
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