Rocks with high total organic carbon, ( termed source rocks ), will alter under increasing temperature such that the organic molecules slowly mature into hydrocarbons ( see diagenesis ).
42.
The solution of metal, salts and water produced by diagenesis is produced at temperatures between 150-350�ppm Zn, Cu, Pb and up to 100ppm Ba and Fe.
43.
This elevated C / N signature is preserved in the sediment, until another form of diagenesis, post-depositional diagenesis, alters its C / N signature once again.
44.
This elevated C / N signature is preserved in the sediment, until another form of diagenesis, post-depositional diagenesis, alters its C / N signature once again.
45.
Calcium carbonate was originally present in the carapaces of trilobites, and may have crystallized early in diagenesis in ( for example ) the guts of " Burgessia ".
46.
When siliceous oozes are incorporated into orogenic belts associated with subduction zones, they are also altered by diagenesis, and lithified to form chert, i . e . radiolarian chert.
47.
In thin section it can be observed that the siliceous groundmass is derived from the innumerable skeletons of radiolarians ( maximal size 0.1 mm in diameter ) altered during diagenesis.
48.
A kinetic model based on experimental data can capture most of the essential transformation in diagenesis, and a mathematical model in a compacting porous medium to model the dissolution-precipitation mechanism.
49.
During diagenesis, pore water is squeezed out of the sediments and, as burial continues and heat increases, water is liberated from clay minerals as the peripheral hydroxyl bonds are broken.
50.
Steranes may be rearranged to diasteranes during diagenesis ( C-27 to C-30, rearrangement at C-18 and C-19, no R at C-24 ).
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