[HTML][HTML] EUNAseis: A seismic model for Moho and crustal structure in Europe, Greenland, and the North Atlantic region

IM Artemieva, H Thybo - Tectonophysics, 2013 - Elsevier
We present a new digital crustal model for Moho depth and crustal structure in Europe,
Greenland, Iceland, Svalbard, European Arctic shelf, and the North Atlantic Ocean (72W …

Glacial rebound and plate spreading: results from the first countrywide GPS observations in Iceland

T Árnadóttir, B Lund, W Jiang… - Geophysical Journal …, 2009 - academic.oup.com
Iceland is one of the few places on Earth where a divergent plate boundary can be observed
on land. Direct observations of crustal deformation for the whole country are available for the …

Compressible magma/mantle dynamics: 3-D, adaptive simulations in ASPECT

J Dannberg, T Heister - Geophysical Journal International, 2016 - academic.oup.com
Melt generation and migration are an important link between surface processes and the
thermal and chemical evolution of the Earth's interior. However, their vastly different …

North Atlantic magmatism controlled by temperature, mantle composition and buoyancy

EL Brown, CE Lesher - Nature Geoscience, 2014 - nature.com
Large igneous provinces are characterized by anomalously high rates of magma production.
Such voluminous magmatism is commonly attributed to partial melting of hot, buoyantly …

The Lebombo monocline and associated feeder dyke swarm: Diagnostic of a successful and highly volcanic rifted margin?

MB Klausen - Tectonophysics, 2009 - Elsevier
As part of the Karoo large igneous province (LIP), the∼ 700 km-long and∼ 182 Ma-old
Lebombo monocline outcrops inland of a younger Mozambique Lowland cover that …

Major influence of plume‐ridge interaction, lithosphere thickness variations, and global mantle flow on hotspot volcanism—The example of T ristan

R Gassmöller, J Dannberg, E Bredow… - Geochemistry …, 2016 - Wiley Online Library
Hotspot tracks are thought to originate when mantle plumes impinge moving plates.
However, many observed cases close to mid‐ocean ridges do not form a single age …

Modelling melting and melt segregation by two-phase flow: new insights into the dynamics of magmatic systems in the continental crust

H Schmeling, G Marquart, R Weinberg… - Geophysical Journal …, 2019 - academic.oup.com
The physics of magmatic systems within continental crust is poorly understood. We
developed a thermomechanical compositional two-phase flow formulation based on the …

[图书][B] Electromagnetic geothermometry

VV Spichak, OK Zakharova - 2015 - books.google.com
Electromagnetic Geothermometry explores, presents and explains the new technique of
temperature estimation within the Earth's interior; the Electromagnetic technique will identify …

The lithosphere and asthenosphere of the Iceland hotspot from surface waves

IT Bjarnason, H Schmeling - Geophysical Journal International, 2009 - academic.oup.com
D models were calculated for the velocity of shear waves, polarized vertically (SV) and
horizontally (SH) from dispersed Rayleigh and Love surface waves. These had been …

Coupled mechanical and hydrothermal modeling of crustal accretion at intermediate to fast spreading ridges

S Theissen-Krah, K Iyer, LH Rüpke… - Earth and Planetary …, 2011 - Elsevier
The genesis of oceanic crust at intermediate to fast spreading ridges occurs by the
crystallization of mantle melts accumulated in at least one shallow melt lens situated below …