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Origin of Island Dolostone: Case Study of Cayman Formation (Miocene), Grand Cayman, British West Indies
DownloadFall 2017
Grand Cayman is located on an isolated fault block that is part of the Cayman Ridge that defines the southern margin of the North American Plate. The exposed part of the Oligocene to Pleistocene carbonate succession that forms the island comprises the Bluff Group (Brac Formation, Cayman...
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Sedimentology, diagenesis, and dolomitization of the Brac Formation (Lower Oligocene), Cayman Brac, British West Indies
DownloadFall 2009
The Oligocene Brac Formation is the oldest part of the Bluff Group that is exposed on Cayman Brac. Sediments of the Brac Formation were deposited on a small, open bank in shallow marine waters. Today, the formation is composed of limestone, finely crystalline dolostone, and coarsely crystalline...
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Spring 2012
This research comprises a series of papers to address the methodology of studying hunter-gatherer mobility in prehistoric populations. As a laboratory for this research, middle Holocene hunter-gatherer groups from Cis-Baikal, Siberia were analyzed as part of ongoing research by the Baikal...
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Spring 2014
The Ironshore Formation, a Pleistocene limestone succession found on Grand Cayman, is formed of six unconformity-bounded units (A to F) that developed in response to transgressive-regressive cycles. Highstands led to deposition whereas lowstands led to diagenetic change in the earlier deposited...