Thermal Development and Rejuvenation of the Marginal Plateaus Along the Transtensional Volcanic Margins of the Norwegian-Greenland Sea

The predominance of large-scale paleo-shear zones in the Norwegian-Greenland Sea is thought to be the major cause of asymmetric seafloor spreading in this region. Plate reconstructions suggest that nascent mid-ocean ridges propagated into these obliquely oriented shear zones causing transtension to...

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Bibliographic Details
Main Author: Okay, Nilgun
Format: Doctoral or Postdoctoral Thesis
Language:English
Published: CUNY Academic Works 1995
Subjects:
Online Access:https://academicworks.cuny.edu/gc_etds/3901
https://academicworks.cuny.edu/cgi/viewcontent.cgi?article=4964&context=gc_etds