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Abstract

Xu and White (1995) developed a practical velocity model for siliciclastic rocks from the Kuster and Toksöz, effective medium and Gassmann theories. In this model, the total pore space is divided into two parts: (1) pores associated with sand grains and (2) pores associated with clays (including bounding water).

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/content/papers/10.3997/2214-4609.201409557
1995-05-29
2024-04-25

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