Geothermal Model of the Fore‐Yenisei Sedimentary Basin– Transitional Structure between the Ancient Siberian Platform and the Young West Siberian Plate
Author:
Affiliation:
1. Trofimuk Institute of Petroleum Geology and Geophysics SB RAS 3, Koptyga ave. Novosibirsk 630090 Russia
2. Novosibirsk State University 1, Pirogov Street Novosibirsk 630090 Russia
Publisher
Wiley
Subject
Geology
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1111/1755-6724.14799
Reference39 articles.
1. Thermal structure of the lithosphere of the siberian platform;Duchkov A.D.;Geologiya i Geofizika,1997
2. Thermal conductivity of the Bazhenovo Formation rocks in the Salym area (West Siberian Plate)
3. Heat flow and geothermal field in Siberia;Duchkov A.D.;Geologiya i Geofizika,1997
4. Thermal conductivity of the sedimentary-cover rocks of the West Siberian Plate in relation to their humidity and porosity
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