Item talk:Q67716
From geokb
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"abstract": "Teapot Dome, Wyoming, also known as National Petroleum Reserve 3, is a candidate for a\nnational CO2 storage test site. The oil field in Upper Cretaceous sandstones at Teapot Dome was\ndiscovered in the 1880's based on surface occurrences of a waxy hydrocarbon, 'ozokerite', within\ncalcite-lined fractures. The goal of this research is to determine if the hydrocarbons resulted from\nactive (i.e. present-day) seepage of the oil reservoirs or from an older episode of local or basinscale\nfluid flow.\nTwo generations of fractures and two separate calcite cementation events are recognized in\noutcrop, and hydrocarbon wax, likely ozokerite, post-dates both calcite generations. The calcite\ncontains two-phase (liquid-vapor), secondary hydrocarbon fluid inclusions that fluoresce a bluewhite\ncolor in UV epi-illumination. The ozokerite also fluoresces blue-white, which suggests that\npetroleum inclusions and the hydrocarbon wax are related. Gas chromatograms (GCs) of ozokerite\nare consistent with GCs of oils from Upper Cretaceous reservoirs at Teapot Dome, indicating that a\nconnection between the fractures and a hydrocarbon reservoir did exist.\nSecondary hydrocarbon inclusions are present in the calcite, which indicates that active oil\nmigration occurred while the fractures were at higher temperatures than surface conditions.\nTherefore, the oil was emplaced within the fractures when they were between 600 to 1500 m deep.\nFurthermore, the ozokerite formed during the uplift and exhumation of the Upper Cretaceous strata\nat Teapot Dome. The fractures in this study have no active connection to any deeper oil-bearing\nstrata.",
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