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Interpretive Processing - Combining Data Driven Velocity Modelling and Geological Knowledge for

机译:解释处理 - 组合数据驱动速度建模和地质知识

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Imaging off the east coast of India poses a specific set of challenges for velocity model building and the migration. Significant topographical variation in the sea bed gives rise to numerous effects which must be dealt with starting with the water velocity that varies with depth and distance from the sub-continent, deep channels and steep slopes, buried channels with low velocity fills and gas hydrates. Deeper down the section one encounters velocity variations introduced by regional unconformities and re-deposition (slumps, canyon cuts and cut and fill areas). The east coast of India has evolved through a multiple cycle of tectonic and sedimentary processes and has been subdivided into several basins. The younger depositional units present a variety of facies ranging from deep marine channel-level to complex canyon fills. In this paper, we describe an approach to tackling such problems for data from the Krishna-Godavari and the Mahanadi Basins off the east coast of India, concentrating our attention on iterative velocity model building, more specifically the resolution of near-seabed and post-Cretaceous velocity anomalies.
机译:在印度东海岸的成像对速度模型建筑和迁移构成了一系列特定的挑战。海面床的显着地形变化产生了许多效果,这些效果必须从水速和距离子大陆,深通道和陡坡的距离变化,埋入速度填充和天然气水合物的埋地通道不同。深入了解一个遇到区域不整合和再沉积(坍落度,峡谷切割和填充和填充区域)引入的速度变化。印度东海岸通过多周期的构造和沉积过程发展,并被细分为几个盆地。年轻的沉积单位呈现出各种相距从深海渠道层到复杂的峡谷填充物。在本文中,我们描述了一种解决克里希纳 - 戈达瓦里和印度东海岸的汉语盆地数据的问题的方法,专注于迭代速度模型建设,更具体地说是近海底和后的分辨率白垩纪速度异常。

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