Model of forming Neocomian clinoform complex of West-Siberian oil-and-gas bearing province with regard to isostasy
It is proposed a mathematical model of forming terrigene filling of Neocomian basin of West Siberia where the basement relief and sedimentary thickness are governed by dynamic isostasy. By model calculation it is demonstrated accumulation of the thick clinoform complex in sea basin of 200-250 m depth accompanied by migration of most downwarping area in west direction.