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Determining continuous basins across conjugate margins: The East Orphan, Porcupine, and Galicia Interior basins of the southern North Atlantic Ocean

机译:南大西洋南部大西洋的东墙,豪猪和加利西亚内部盆地中的连续盆地

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摘要

The East Orphan, Porcupine, and Galicia Interior basins are several of the most promising basins for hydrocarbon exploration along the rifted continental margins of the southern North Atlantic Ocean. Despite having formed at similar geological times, the basins exhibit fundamental differences in symmetry, crustal thickness, sedimentary cover thickness, and amount of extension. Interpretation of seismic reflection and well data was integrated with published 3D grids of depth-to-basement and Moho proxy depth to interpret and restore select seismic reflection lines. Publicly available kinematic evolution models were also integrated to evaluate and compare the restored seismic reflection lines in a more global regional context.
机译:东侧孤儿,豪猪和加利西亚内部盆地是沿着北大西洋南部大西洋的裂缝勘探中最有前途的盆地中最有前途的盆地。 尽管形成了类似的地质时间,但盆地表现出对称性,地壳厚度,沉积覆盖厚度和延伸量的根本差异。 地震反射和井数据的解释与发布的3D电网与深度到地下室和Moho代理深度的诠释,以解释和恢复选择地震反射线。 还集成了公开可用的运动进化模型来评估和比较更全球区域背景下的恢复的地震反射线。

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