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| Factory | Dominant Mineral | Typical Setting | Example | |---------|----------------|----------------|---------| | (chlorozoan) | Aragonite, high-Mg calcite | Shallow, warm (<30° latitude) | Great Bahama Bank | | Cool-water (foramol) | Low-Mg calcite | Mid-latitudes, temperate | Southern Australia shelf | | Mud-mound (microbial) | Micrite, authigenic clays | Deep ramp, dysoxic | Devonian of Canning Basin |
This evolutionary context is critical; an Ordovician limestone originates from different biological and chemical processes than a modern Bahamian ooid shoal. origin of carbonate sedimentary rocks pdf extra quality
of specific chemical grades, or would you like to dive deeper into the geographic locations where these high-purity deposits are mined? | Factory | Dominant Mineral | Typical Setting