... according to the temperature structure beneath the Kurile Island Arc after the model by Honda aamp; Uyeda (1983), along with ... the layers l-3A takes place beneath the frontal zone, while dehydration of serpentine from the layer 3B occurs beneath the rear zone. ... Our analysis of the structures of this segment of the Alpine belt has revealed that its development took place in a considerably different way.
|Title||:||L.P. Zonenshain Memorial Conference on Plate Tectonics|
|Author||:||L.P. Zonenshain Laboratory of Paleogeodynamics, Research Center for Marine Geosciences|