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Step 5 Calculation of compaction history.
However, using just two lithologies is an oversimplification that cannot represent the compaction history.
The assessment of the differential compaction history of clastic rocks eliminates the effects of compaction-induced subsidence which determine unwanted overestimation of slip rates.
Such a method is not able to represent and generalize the compaction history of mixed grain-size lithologies such as muddy siltstone and silty mudstone, in addition to pure mudstone and pure sandstone.
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In this way, the rock-physics experiments illustrate that lithologically independent compaction histories can be identified based on clay content.
From the petrography of the samples, the basin shows complex diagenetic histories which include compaction, cementation/micritization, dissolution, overgrowth of quartz, and fracturing.
Mechanical compaction lasted through the entire diagenetic history.
Factors that influence specific gravity were investigated including waste particle size, compaction, and combined decomposition and stress history.
It's used to test the compaction of recently compacted roads.
For example the Ala119Thr substitution was identified in a family with a history of DCM, left ventricular non-compaction, idiopathic ventricular fibrillation and unexplained sudden death [ 44].
This study revealed a complex diagenetic history of sandstones of the Orange Basin in which compaction, cementation/micritization, dissolution, overgrowth of quartz and fracturing were observed.
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