Titlebook: Geology of the Cayman Islands; Evolution of Complex Brian Jones Book 2022 The Editor(s) (if applicable) and The Author(s), under exclusive

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Digital Logic Design Using Verilogare echinoids. There are, however, only scattered, small coral patch reefs. Fossil-mouldic porosity is common given that the aragonitic skeletons of the corals and other organisms were commonly lost during early diagenesis. The dolostones, characterized by high porosity (up to 48%), are commonly cut

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https://doi.org/10.1007/978-3-319-56839-3hytokarst surfaces on the Pedro Castle Formation are generally more subdued than those on the Cayman Formation because the limestones–dolostones are not as hard as those in the Cayman Formation. The dolostones are typically formed of anhedral to euhedral dolomite crystals that are mostly <50?μm long

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Introducing Online Brand Communities,the late 1800s. The phosphates that remain on Little Cayman are mostly formed of hydroxylapatite with boehmite and crandallite being present locally. These deposits, formed largely of P.O., CaO, Al.O., Fe.O., and MnO, are petrographically complex with various admixtures of lithoclasts, coated grains

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no longer exist). Most samples have been fully documented petrographically and geochemically..Data from 120 wells that have been drilled to depths up to 245 m (most less than 125 m). Wells have been cored and/978-3-031-08232-0978-3-031-08230-6

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,Bluff Group—the Brac Formation,lostones (zoned euhedral crystals up to 1.5?mm long) that are characterized by numerous different diagenetic stages that included the development of limpid dolomite cements, calcite cements, and complex vadose cements formed of calcite and dolomite. The Brac Formation on Grand Cayman is poorly under