The thermal evolution of solid bitumens, bitumen reflectance, and kinetic modeling of reflectance: application in petroleum and ore prospecting

Abstract This article is concerned with (1) the prevailing chemical processes involved in the thermal evolution of sulfur-rich and -poor solid bitumens, represented by the “type locality” wurtzilite and albertite, (2) the reflectance evolution of solid bitumens and its relationship to vitrinite reflectance, and (3) the application of bitumen reflectance and bireflectance in estimating the palaeothermal conditions in the petroleum- and ore-bearing sediments. The thermal evolution of wurtzilitelike bitumens will result in depolymerization and formation of petroleum-soluble molecules. The thermal evolution of albertite will result in the formation of increasingly condensed, petroleum-insoluble residues. Broadly speaking, the response of albertitelike bitumens to maturity increase is similar to that of kerogen. A kinetic model of relevance to petroleum exploration, calibrated by geological and laboratory data, was designed. The model shows that the bitumen-vitrinite reflectance relationship is insensitive to ...

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