Abstract
According to the results of a comprehensive sedimentological study of the core and well log data, the dissection of the bat-upper Jurassic sediments of the South of the West Siberian oil and gas basin was carried out. Quasi-isochronous marked levels are identified. They are represented by transgressive surfaces, maximum flooding surfaces and extended carbonaceous layers. They are the basis of the performed correlation. A number of characteristic lithological-facies sequences diagnosed by well log data was established.
Highlights
По результатам комплексного седиментологического исследования керна и материалов ГИС проведено расчленение разрезов бат-верхнеюрских отложений юга Западно-Сибирского нефтегазоносного бассейна
Quasi-isochronous marked levels are identified. They are represented by transgressive surfaces, maximum flooding surfaces and extended carbonaceous layers
They are the basis of the performed correlation
Summary
ИНТЕРПРЕТАЦИЯ ДАННЫХ ГИС ПРИ ПАЛЕОГЕОГРАФИЧЕСКИХ РЕКОНСТРУКЦИЯХ (НА ПРИМЕРЕ БАТ-ВЕРХНЕЮРСКИХ ОТЛОЖЕНИЙ ЮГА ЗАПАДНОЙ СИБИРИ) По результатам комплексного седиментологического исследования керна и материалов ГИС проведено расчленение разрезов бат-верхнеюрских отложений юга Западно-Сибирского нефтегазоносного бассейна. Муромцев опробовал разработанные приемы анализа материалов ГИС на более сложных объектах, в том числе и в Западной Сибири.
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