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Genesis and geometry of the Meiklejohn Peak lime mud-mound, Bare Mountain Quadrangle, Nevada, USA: Ordovician limestone with submarine frost heave structures—a possible response to gas clathrate hydrate evolution

Basin EvolutionBare Mountain QuadrangleEngineeringStructural GeologyGeomorphologyBasin AnalysisNatural Gas Hydrate SystemGeographySedimentary GeologyRegional GeologySubmarine FrostGeologyPetrologySedimentologyEarth ScienceOrdovician LimestoneRock PropertiesTectonics