Veined pyrobitumen in dolerites of the Kuzmensky complex - (Minusa intermontane trough)

Veined pyrobitumen in dolerites of the Kuzmensky complex - (Minusa intermontane trough) Full article

Journal

Геология и геофизика
ISSN: 0016-7886

Output data

Year: 2001, Volume: 42, Number: 7, Pages: 1110-1117 Pages count : 8

Tags

pyrobitumens; IR spectra; pyrolysis; dolerite sills; Minusa intermontane trough

Authors

Fedoseev GS , Fadeeva VP , Melenevsky VN

Affiliations

1	(Данные Web of science) Russian Acad Sci, Inst Geol, Novosibirsk 630090, Russia
2	(Данные Web of science) Novosibirsk Organ Chem Inst, Novosibirsk 630090, Russia
3	(Данные Web of science) Siberian Geol Geophys & Mineral Resources Res Ins, Novosibirsk 630091, Russia

Study of solid natural hydrocarbons is of great theoretical and practical importance. On the one hand, their industrial accumulations may be considered a nontraditional raw-material source for chemical industry. On the other hand, they permit us to solve problems on formation of by-products of naphthidogenesis. In this paper we describe hard bitumens ("pyrobitumens") localized within dolerite sills and report evidence of the destructive-sublimation character of their formation simultaneous with sill genesis in the Minusa Intermontane trough.

Fedoseev G. , Fadeeva V. , Melenevsky V.
Veined pyrobitumen in dolerites of the Kuzmensky complex - (Minusa intermontane trough)
Геология и геофизика. 2001. V.42. N7. P.1110-1117. WOS РИНЦ

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