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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Format: | Doctoral or Postdoctoral Thesis |
Language: | English |
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CUNY Academic Works
1995
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Online Access: | https://academicworks.cuny.edu/gc_etds/3901 https://academicworks.cuny.edu/cgi/viewcontent.cgi?article=4964&context=gc_etds |