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The values for clastic sedimentary rocks would be particularly variable.
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To date, this oxidation effect has only been documented for clastic sediments rich in iron.
At depocenter scale, overburden vertical movements due to salt evacuation or salt diapiric rise create sub-basins, providing accommodation space for clastic deposition.
This dependence (or hysteresis) is particularly important for water-alternating-gas (WAG) injection, a successful CO2 EOR and storage method for clastic and carbonate reservoirs.
The relationships between compressional wave and shear wave velocities were discussed by Castagna et al. 1985 for clastic silicate rocks.
This model has been validated, with the assumptions valid for clastic reservoirs such as those in the Niger Delta basin.
We have used mudrock line for clastic silicate rock (Castagna et al. 1985), which is often used to evaluate the V p and V s in marine sediments.
It should be noted that mud loss mechanisms described above are mainly for clastic formations but may not be relevant to carbonate formations.
The resulting multilevel fault terrace belts not only created multilevel delivery paths for clastic transportation, but also controlled the distribution of depositional facies from a shallow water into a deep lake environment (Hou et al. 2012) (Fig. 7).
Depositional settings and their effects on reservoir quality are of particular interest for clastic reservoirs, where contemporaneous salt movement influences sedimentation and the resulting distribution of facies (e.g. Fox 1998; Banham and Mountney 2013a, b).
Values for triplicates were averaged.
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