Abstract:Salt tectonics is typically caused by the flow of mobile evaporites in response to postdepositional gravity gliding and/or differential loading by overburden sediments. This situation is considerably more complex near the margins of salt basins, where carbonate and clastic rocks may be deposited at the same time and interbedded with, more mobile, evaporite strata. In these cases, syn-depositional salt flow may occur due to density differences in the deposited lithologies, although our understanding of this pro… Show more
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