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Chemofossils in oils and rocks in the Bazhenovo Formation at the Salym field

Journal Article · · Int. Geol. Rev.; (United States)

No unambiguous explanation has so far been given for the origin of oil pools in the Bazhenovo formation, although most investigators consider that the Bazhenovo oil to be autochthonous, that is, due to thermal destruction of dispersed organic matter. However, some investigators assume an allochthonous origin for the pools, with the hydrocarbons migrating from older beds along faults. The model chosen governs the exploration strategy, so establishing the source is a matter of practical as well as theoretical importance. Chemofossils are widely used, including the n-alkanes, carboxylic acids, and aliphatic isoprenoids, in particular pristane C/sub 19/ and phytane C/sub 20/. The relict hydrocarbon distributions are affected not only by the composition of the initial organic matter but also by the deposition conditions (Eh and pH), stratal mineral compositions, and catagenesis, which is dependent mainly on the stratal temperatures. Here the authors not only compare these chemofossils in the Salym oils and rocks but also analyze the pristane and phytane distributions in relation to T/sub st/ and consequent thermal effects on the organic and mineral matter of the rock. The authors examined the relict hydrocarbons by chromatography and chromatography-mass spectroscopy. 13 references.

OSTI ID:
6962094
Journal Information:
Int. Geol. Rev.; (United States), Journal Name: Int. Geol. Rev.; (United States) Vol. 29:9; ISSN IGREA
Country of Publication:
United States
Language:
English