APPLICATION OF DIAMONDOIDS TO DISTINGUISH SOURCE ROCK FACIES

dc.contributor.author	Schulz L.K.
dc.contributor.author	Wilhelms A.
dc.contributor.author	Rein E.
dc.contributor.author	Steen A.S.
dc.date.accessioned	2021-02-11T07:53:54Z
dc.date.available	2021-02-11T07:53:54Z
dc.date.issued	2001
dc.identifier	https://www.elibrary.ru/item.asp?id=564623
dc.identifier.citation	Organic Geochemistry, 2001, 32, 3, 365-375
dc.identifier.issn	0146-6380
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/24655
dc.description.abstract	Diamondoid distributions in solvent extracts from marine siliciclastic shales, marine carbonates, and coals of a wide variety of maturities were determined by GC-MSD. For this sample set, published diamondoid maturity parameters did not change systematically throughout the oil window. It was found that several novel diamondoid ratios were indicative of source. It was possible to distinguish between terrigenous, marine carbonate and marine siliciclastic facies. The proposed dimethyl diamantane facies ratios are virtually unaffected by maturity, while the ethyl adamantane ratio appears to be affected by maturity in the late gas-window range.
dc.subject	DIAMONDOID HYDROCARBONS
dc.subject	SOURCE ROCKS
dc.subject	FACIES
dc.subject	MATURITY
dc.subject	OIL CORRELATION
dc.title	APPLICATION OF DIAMONDOIDS TO DISTINGUISH SOURCE ROCK FACIES
dc.type	Статья

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