Rock acoustics of diagenesis and cementation
Jos\'e M. Carcione, Davide Gei, Stefano Picotti, Ayman N. Qadrouh,, Mamdoh Alajmi, Jing Ba

TL;DR
This study models how diagenesis, cementation, and compaction affect the elastic properties of shales and sandstones, providing a simple method to predict seismic velocities based on geological processes and temperature history.
Contribution
It introduces a basin-evolution model integrating four petro-elastical theories to simulate elastic property changes during diagenesis and cementation, accounting for mineral transformations and effective pressure effects.
Findings
Seismic velocities increase with depth and temperature.
Different petro-elastical models produce similar velocity predictions.
The methodology enables velocity estimation based on geological history.
Abstract
We simulate the effects of diagenesis, cementation and compaction on the elastic properties of shales and sandstones with four different petro-elastical theories and a basin-evolution model, based on constant heating and sedimentation rates. We consider shales composed of clay minerals, mainly smectite and illite, depending on the burial depth, and the pore space is assumed to be saturated with water at hydrostatic conditions. Diagenesis in shale (smectite/illite transformation here) as a function of depth is described by a 5th-order kinetic equation, based on an Arrhenius reaction rate. On the other hand, quartz cementation in sandstones is based on a model that estimates the volume of precipitated quartz cement and the resulting porosity loss from the temperature history, using an equation relating the precipitation rate to temperature. Effective pressure effects (additional…
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