Structural and Geochemical Interactions Between Magma and Sedimentary Host Rock: The Hovedøya Case, Oslo Rift, Norway

Structural and Geochemical Interactions Between Magma and Sedimentary Host Rock: The Hovedøya Case, Oslo Rift, Norway

Abstract Two end‐member conceptual models are used to describe deformation of the Earth's crust induced by magma intrusion. “Mode I” fracturing assumes tensile or opening‐mode, elastic deformation, while “Mode II” fracturing assumes plastic shear‐mode deformation around a viscous indenter. Fiel...

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Bibliographic Details
Main Authors: S. Poppe, O. Galland, N. J. deWinter, S. Goderis, P. Claeys, V. Debaille, P. Boulvais, M. Kervyn
Format: Article
Language:English
Published: Wiley 2020-03-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
magma
intrusion
structural deformation
Oslo Rift
geochemistry
stable isotopes
Online Access:https://doi.org/10.1029/2019GC008685

Internet

https://doi.org/10.1029/2019GC008685

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