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Transgressive-regressive cycles in the Ironshore Formation, Grand Cayman, British West Indie

Posted on:2004-05-31Degree:M.ScType:Thesis
University:University of Alberta (Canada)Candidate:Coyne, Morag KathleenFull Text:PDF
GTID:2460390011967872Subject:Geology
Abstract/Summary:
Most studies of Caribbean carbonate deposits measure sea level in relation to established highstands. In this study, however, examination of the Ironshore Formation on Grand Cayman revealed a succession of 6 units (A, B, C, D, E, and F) whose deposition ages correlate to transgressive-regressive sea level cycles. The two youngest units, E and F, were discovered during the course of this study. Onshore and offshore fossil dates established that Unit D ranges in age from 123 to 147 ka (average133 ka), Unit E from 95 to 110 ka (average 101 ka), and Unit F from 80 to 87 ka (average 80 ka). Unit D was deposited during the transgression that led to the Sangamon highstand. Units E and F were deposited throughout the transgressive and regressive cycles of substages 5c and 5a, respectively.
Keywords/Search Tags:Cycles, Unit
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