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f Geology, organic geochemistry and hydrocarbon reserves in the Arctic Zone of the West Siberian Basin
- Publisher: European Association of Geoscientists & Engineers
- Source: Conference Proceedings, 55th EAEG Meeting, Jun 1993, cp-46-00386
- ISBN: 978-94-6282-135-4
Abstract
The Arctic Zone of the West Siberian basin includes the Yamal-Taz megasyncline and Southern Kara sea megatrough. This area occupies more than 1,200,000 km². The Yamal-Taz megasyncline devides the Yamal-Gydan and Nadym-Taz Sineclines, the Yenisey-Khatanga megatrough, and Messoyakha belt swells. Giant gas-condensate fields located on the megaswells system are: Kharasaveye - Novyy Port, Northern Yamal, Yamburg - Medvezhye, Urengoy and Russko-Chaselskeye. The active growth of this tectonic elements have taken place in Neokomian and Cenozoic times. West- East extention in late Permian to Early Triassic time created the main rift systems: West Omsk - Yamal and East Omsk - Urengoy - Cydan.