Structure and depositional environment of the Vasyugan Horizon (Upper Bathonian-Oxfordian) in the Aleksandrovskoe arch area (West Siberia)


статья в журнале
Авторы: Vakulenko L.G.   (ИНГГ СО РАН)   Dul'tseva O.V.   (ИНГГ СО РАН)   Burleva O.V.   (ИНГГ СО РАН)  
дата публикации: 2011
реферат:
An integrated sedimentological study of the Vasyugan Horizon in the Aleksandrovskoe arch area was performed, during which its depositional environments were reconstructed and a series of paleogeographic maps was plotted. It has been established that shallow-marine, marginal-marine, transitional, and continental depositional environments existed here at various stages. Most of the arch area is characterized by sections of the transitional Naunak-Vasyugan and Vasyugan-Naunak types; the westernmost part, by sections of the Vasyugan type, and the easternmost part, by sections of the Naunak type. The sand beds of the J1 horizon are low-quality reservoirs, whereas those on the western slope and the northern pericline of the Aleksandrovskoe arch are of better quality.
первоисточник: Russian Geology and Geophysics
том: 10
страницы: 1212-1227
ISBN:
ISSN:
внешние ссылки:
WoS   WoS (цитирование)
DOI  
РИНЦ SPIN  
Scopus  

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полный текст статьи

rgg-2011-10-1212