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Joint inversion of gravity and multiple components of tensor gravity data

机译:重力和张量重力数据的多个分量的联合反演

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Geological structures often exhibit smooth characteristics away from sharp discontinuities. One aim of geophysical inversion is to recover information about the smooth structures as well as about the sharp discontinuities. Because no specific operator can provide a perfect sparse representation of complicated geological models, hyper-parameter regularization inversion based on the iterative split Bregman method was used to recover the features of both smooth and sharp geological structures. A novel preconditioned matrix was proposed, which counteracted the natural decay of the sensitivity matrix and its inverse matrix was calculated easily. Application of the algorithm to synthetic data produces density models that are good representations of the designed models. The results show that the algorithm proposed is feasible and effective.
机译:地质结构通常表现出平滑的特征,而没有尖锐的不连续性。地球物理反演的一个目的是恢复有关光滑结构以及尖锐不连续面的信息。由于没有专门的算子可以提供复杂地质模型的完美稀疏表示,因此基于迭代分裂Bregman方法的超参数正则化反演被用于恢复光滑和尖锐地质结构的特征。提出了一种新的预处理矩阵,该矩阵可以抵消灵敏度矩阵的自然衰减,并且可以容易地计算其逆矩阵。将算法应用于合成数据会产生密度模型,这些密度模型很好地表示了设计模型。结果表明,该算法是可行和有效的。

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