Geological Backgrounds Of Siberian Traps
The Siberian Carton is old, cold and thick,
unlike the much younger lithosphere of the WSB, which is young, thin and
hot. Furthermore, whereas the Carton has remained stable since the
Permian (and probably for a long time before that), the Paleozoic
surface of the West Siberian Basin has subsided.
Not only has this
resulted in deep burial of the basaltic sequences, but it has helped
create substantial oil and gas fields - some of the world's largest
(Peterson and Clarke, 1991).