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Eustatic and Tectonic Controls on the Development of the Stratigraphic Architecture of the Cayman Islands, British West Indies
DownloadFall 2019
The Paleogene to Neogene carbonate sedimentary successions that form the cores of each of the Cayman Islands, which are located within 150 km of each other, developed on isolated banks that were surrounded by deep oceanic water. Although each of the Cayman Islands has experienced uniform changes...
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