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Crosswell tomographic estimation of elastic constants in heterogeneous transversely isotropic media

机译:非均质横向各向同性介质中弹性常数的Crosswell层析成像估计

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The procedure to estimate elastic constants of a transversely isotropic medium from limited-aperture traveltimes has two steps. First, P- and SV-wave traveltimes are fitted with elliptical velocity functions around one of the axes of symmetry. Second, the parameters that describe the elliptical velocity functions are transformed analytically into elastic constants. When the medium is heterogeneous, the process of fitting the traveltimes with elliptical velocity functions is performed tomographically, and the transformation to elastic constants is performed locally at each position in space. Crosswell synthetic and field data examples show that the procedure is accurate as long as the data aperture is constrained as follows: it should not be too large otherwise the elliptical approximation may not be adequate, and it should not be too small because the tomographic estimation of elliptical velocities fails, even if the medium is actually isotropic.
机译:从有限孔径的传播时间估计横向各向同性介质的弹性常数的过程有两个步骤。首先,P波和SV波的传播时间在对称轴之一周围装有椭圆速度函数。其次,将描述椭圆速度函数的参数解析地转换为弹性常数。当介质是非均质的时,以层析速度执行将行程时间与椭圆速度函数拟合的过程,并在空间中的每个位置局部执行对弹性常数的转换。 Crosswell合成数据和现场数据示例表明,只要按以下方式限制数据孔径,该过程就很准确:它不应太大,否则椭圆近似值可能不足够,并且它也不能太小,因为对X射线的层析成像估计即使介质实际上是各向同性的,椭圆速度也会失败。

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