Advective-polymorphous process in the tectonosphere of a transition zone of atlantic type
© Gordienko V.V.
The geological history of the transition zone of Atlantic type is considered. A scheme of deep processes taking place in the tectonosphere of the transition zone that corresponds with ideas of polymorphous - advection hypothesis has been set up. The correspondence of the known processes in the subsurface layer of the crust with those predicted by the hypothesis is shown. The agreement of the data on physical fields with the calculated ones is demonstrated. <<back |
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