Titlebook: Geodynamics of Iceland and the North Atlantic Area; Proceedings of the N L. Kristjansson Conference proceedings 1974 D. Reidel Publishing C

發(fā)炎

interlude

Vertical Crustal Movement in Iceland,iated with this subsidence is characterized by gentle bending of the earth’s crust with no measureable fault displacement except during earthquakes and possibly during a period of one or two years after earthquakes.

辯論的終結(jié)

deforestation

https://doi.org/10.1007/978-3-531-92487-8ich is anomalously high compared to other oceans of comparable age. Measurements at distances greater than 100 km from the Reykjanes Ridge axis show a steady decrease with age, and when age is taken into account the heat flow is also anomalously high relative to other spreading centers.

debris

Marine Heat Flow Measurements in the Norwegian-Greenland Sea and in the Vicinity of Iceland,ich is anomalously high compared to other oceans of comparable age. Measurements at distances greater than 100 km from the Reykjanes Ridge axis show a steady decrease with age, and when age is taken into account the heat flow is also anomalously high relative to other spreading centers.

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