Consolidation (geology)

In this article, the topic of Consolidation (geology) will be addressed from a broad and detailed perspective. Through an exhaustive analysis, different aspects related to Consolidation (geology) will be explored, including its origin, evolution and relevance today. Different points of view, theories and studies on Consolidation (geology) will be examined, in order to provide a comprehensive and enriching vision on this topic. In addition, concrete examples and practical cases will be analyzed that illustrate the importance and influence of Consolidation (geology) in different contexts. Finally, reflections and conclusions will be proposed that invite readers to deepen their understanding and appreciation of Consolidation (geology).

In geology, consolidation is used in several senses:

• Lithification, the overall process of conversion of loose sediments to solid rock.
• Any other process in which loose or fluid material becomes solid rock, such as solidification of magma.
• Compaction (geology), the decrease in volume and increase in density of sediments as the weight of overlying sediments increases, mineral grains move to more compact arrangements, and pore water is expelled. The term is particularly used for soil consolidation.
• Rarely, as a term for the conversion of a mobile belt to a rigid part of a continental platform; an orogeny.

References

1. ^ ^{a b c d} Jackson, Julia A., ed. (1997). "consolidation". Glossary of geology (Fourth ed.). Alexandria, Virginia: American Geological Institute. ISBN 0922152349.
2. ^ ^{a b} Allaby, Michael (2013). A dictionary of geology and earth sciences (Fourth ed.). Oxford: Oxford University Press. ISBN 9780199653065.

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