Creep of mafic dykes infiltrated by melt in the lower continental crust (Seiland Igneous Province, Norway)

A dry mafic dyke from a continental lower-crustal shear zone in the Seiland Igneous Province (northern Norway) experienced syn-kinematic melt-rock interaction. Viscous shearing occurred at T ≈ 800 °C, P ≈ 0.75–0.95 GPa and was coeval with infiltration of felsic melt from adjacent migmatitic metapeli...

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Bibliographic Details
Published in:Lithos
Main Authors: Degli Alessandrini, G, Menegon, L, Malaspina, N, Dijkstra, A, Anderson, M.
Other Authors: Anderson, M
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier B.V. 2017
Subjects:
Online Access:http://hdl.handle.net/10281/141779
https://doi.org/10.1016/j.lithos.2016.12.030
http://www.sciencedirect.com/science/article/pii/S0024493716304650