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Published in 2017 at "Lithos"
DOI: 10.1016/j.lithos.2016.12.030
Abstract: Abstract 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…
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Keywords:
fine grained;
mafic;
igneous province;
seiland igneous ... See more keywords