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The 2–10‐km‐thick, mainly carbonate cap of the 14,000 km² Bahamas carbonate platform (BCP) has impeded imaging of its underlying crustal structure. The deeper structure of the BCP records both its Mesozoic rift and hotspot history and its later deformation related to its Paleogene collision with the Great Arc of the Caribbean (GAC). We use regional...
Thesis (Ph. D.)--University of Texas at Austin, 1972. Includes vita. Bibliography: leaves 142-146. Microfilm. s
