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diapirism

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diapirism

Geological process in which a particularly light rock, such as rock salt, punches upwards through the heavier layers above. The resulting structure is called a salt dome, and oil is often trapped in the curled-up rocks at each side.



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Most Maykopian outcrops are tied with phenomena of diapirism, which have caused the deposits to be in the surface or down along the kernels of numerous diapiric folds.
GC234 and GB425 are in the geologically and bathymetrically complex Garden Banks and Green Canyon regions characterized by active salt diapirism, associated faulting (Bouma et al.
1982, On the mechanisms of igneous diapirism, stoping and zone melting: American Journal of Science, v.
 
 
 
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