Reutilisation of hydrothermal vent complexes for focused fluid flow on continental margins (Modgunn Arch, Norwegian Sea)
Author:
Affiliation:
1. 3D Seismic Lab School of Earth and Ocean Sciences Cardiff University Cardiff UK
2. Timelapsegeo AS Trondheim Norway
3. formerly at Department of Geoscience and Petroleum Norwegian University of Science and Technology Trondheim Norway
Funder
Natural Environment Research Council
Publisher
Wiley
Subject
Geology
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1111/bre.12507
Reference65 articles.
1. 6403/6‐1. (2008). Retrieved from Factpages Norwegian Petroleum Directorate website:https://factpages.npd.no/factpages/Default.aspx?culture=no
2. 6405/7‐1. (2005). Retrieved from Factpages Norwegian Petroleum Directorate website:https://factpages.npd.no/factpages/Default.aspx?culture=no
3. Contact metamorphism and thermogenic gas generation in the Vøring and Møre basins, offshore Norway, during the Paleocene–Eocene thermal maximum
4. Devolatilization-induced pressure build-up: Implications for reaction front movement and breccia pipe formation
5. Contact metamorphic devolatilization of shales in the Karoo Basin, South Africa, and the effects of multiple sill intrusions
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