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Abstract

The Marrat Formation of Pliensbachian to Toarcian age was deposited in Kuwait as part of regionally widespread carbonateevaporite platform that gently sloped to the east. The formation occurs at a depth of 15500-17050 feet and its thickness varies from 580 feet to 700 feet in the area of study. It is overlain by Dharuma formation and underlain by Minjur formation.

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/content/papers/10.3997/2214-4609-pdb.287.1212883
2012-03-04
2024-03-28
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.287.1212883
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