Geology Reference
In-Depth Information
configurations, the configurations tending more to reflect the history of formation
than the influence of the thermodynamic factors discussed above and so making
generalization difficult. Commonly voids will represent space occupied during the
genesis of the rock by aqueous fluids since lost or space formed by microcracking
under external or internal stresses, and they may be re-filled in various degrees by
material deposited later. Microcracks may also be transgranular and other pores
such as fluid inclusions may be found within grains. For further information, see
David et al. (
1999
).
References
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