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Transport of Geothermal Fluids along Dikes and Fault Zones
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Land og synir: An Interview with Ágúst Guðmundsson
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Transport of Geothermal Fluids along Dikes and Fault Zones
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Model Investigations of a Juvenile Fish Bypass System at Urriðafoss HEP
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Entropies and Scaling Exponents of Street and Fracture Networks
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Iceland's Arctic Strategy. Security challenges and opportunities
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Entropies and Scaling Exponents of Street and Fracture Networks
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Stratigraphy and paleomagnetism of a 3-km-thick Miocene lava pile in the Mjoifj�...
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Stratigraphy, palaeomagnetism and age of volcanics in the upper regions of ÞJórs...
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Stratigraphy and paleomagnetism of a 2.9-km composite lava section in Eyjafj�rdu...
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Stratigraphy and paleomagnetism of a 2.9-km composite lava section in Eyjafj�rdu...
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Assessment and Prediction – Long-term Observation of Icelandic Volcanoes and Gla...
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The regional distribution of mountain permafrost in Iceland
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The Distribution, Thermal Characteristics and Dynamics of Permafrost in Tröllask...
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Age and magnetism of lavas in Jökuldalur area, Eastern Iceland: Gilsá event revi...
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Age and magnetism of lavas in Jökuldalur area, Eastern Iceland: Gilsá event revi...
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Age and magnetism of lavas in Jökuldalur area, Eastern Iceland: Gilsá event revi...
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Limited glaciation and very early deglaciation in central Iceland Implications f...
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Related Subjects
Igneous
Years BP
Lava
Porphyritic Basalt
Tholeiite
3430000
60000
Basalt
Basaltic Lava
Extrusive
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5000000
9000000
Basaltic Andesite
Darcy’s law
Rhyolite
entropy
fault core
fault damage zone
fracture networks
geothermal systems
intrusions
permeability
power laws
scaling exponents
street networks
10500000
13500000
2060000
930000
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