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A method for gravity and magnetic data inversion using vector and tensor data with seismic imaging and geopressure prediction for oil, gas and mineral exploration and production

机译:一种利用矢量和张量数据结合地震成像和地压预测进行重力和磁数据反演的方法,用于石油,天然气和矿物勘探和生产

摘要

A method for modeling geological structures includes obtaining seismic data and using these data to derive an initial density model. Potential fields data is used to update the initial geophysical model by an inversion process using vector or tensor components of gravity and/or magnetic data. In regions having an anomalous density zone, the initial model includes a topographic or bathymetric surface and a 2D or 3D density model including the top of any zones of anomalous density. Potential fields data is then used to derive the lower boundary of the anomalous density zones by using an inversion process. The final density model from the inversion may be further refined using the seismic data in conjunction with the model obtained by inversion of the potential fields data. The model data are integrated two or three dimensions to determine an overburden stress for the subsurface that includes a proper treatment of the anomalous density zone. In an optional process, the seismic data can be processed in depth or time using the density model from the inversion to improve the quality of the velocity information adjacent to and beneath the anomalous bodies.
机译:一种用于对地质结构进行建模的方法,包括获取地震数据并使用这些数据得出初始密度模型。势场数据用于通过重力和/或磁数据的矢量或张量分量的反演过程来更新初始地球物理模型。在具有异常密度区域的区域中,初始模型包括地形或测深表面以及2D或3D密度模型,其中包括任何异常密度区域的顶部。然后使用反演过程将势场数据用于导出异常密度带的下边界。反演的最终密度模型可以结合地震数据和通过势场数据反演获得的模型进一步完善。对模型数据进行二维或三维积分,以确定包括适当处理异常密度区在内的地下超负荷应力。在可选过程中,可以使用反演中的密度模型在深度或时间上处理地震数据,以提高异常体附近和下方的速度信息的质量。

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