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Origin of island dolostones: case study based on Tertiary dolostones from Cayman Brac, British West Indies
DownloadSpring 2013
Cayman Brac (19 km long, 1.5 to 3 km wide), which is the easternmost of the Cayman Islands, is characterized by a thick Tertiary carbonate succession that has been pervasively dolomitized. The finely crystalline dolostones in the Cayman Formation (Miocene) are fabric-retentive whereas the...
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