© 1977 American Geophysical Union THE BAIE VERTE LINEAMENT, NEWFOUNDLAND: OPHIOLITE COMPLEX FLOOR AND
is a steeply-dipping linear belt 90 km long by 1 to 5 km wide containing a variably disrupted ophiolite suite and other mainly mafic volcaniclastic and volcanic rocks that originally overlay the ophiolite complex. The ophiolite complex closely resembles others interpreted as samples of oceanic crust...
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Language: | English |
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.575.6807 http://www.atmos.albany.edu/facstaff/wkidd/Kidd77AGUmev1.pdf |