Abstract

Following the discovery of large volumes of hydrocarbons in the Cordilleran thrust belt of southwestern Wyoming and northern Utah, Angevine and Turcotte (1983), Edman and Surdam (1984), and Furlong and Edman (1984) discussed the role of thrust faulting in hydrocarbon generation. The authors concluded that overthrusting plays an important or even dominant role in the process of hydrocarbon generation in overthrust terrains. These conclusions may be in error because they are based on a mathematical analysis of thermal and geologic models that have little resemblance to actual thrust-belt geology. In this discussion, the authors discuss shortcomings of the thermal model used in the papers referred to above; emphasize the differences between their model and the geologic facts as they exist in thrust belts in general and in western Wyoming in particular; and caution readers about applying the conclusions based on such a model in the search for hydrocarbons. They contend that the temperature effects of thrust faulting were rather insignificant in the process of hydrocarbon generation in the Wyoming thrust belt.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.