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

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

Журнал

Геология и геофизика
ISSN: 0016-7886

Вых. Данные

Год: 2001, Том: 42, Номер: 7, Страницы: 1110-1117 Страниц : 8

Ключевые слова

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

Авторы

Fedoseev GS , Fadeeva VP , Melenevsky VN

Организации

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

Web of science	WOS:000171458300009
РИНЦ	31310350