Rocks from the Gibbs fracture zone and the Minia seamount near 53°N in the Atlantic Ocean
- 31 January 1973
- journal article
- Published by Elsevier in Marine Geology
- Vol. 14 (1) , 47-72
- https://doi.org/10.1016/0025-3227(73)90042-x
Abstract
No abstract availableKeywords
This publication has 26 references indexed in Scilit:
- Flow through the Charlie-Gibbs Fracture Zone, Mid-Atlantic RidgeCanadian Journal of Earth Sciences, 1972
- Metamorphism in the Mid-Atlantic Ridge near 24° and 30° NPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1971
- Petrology of a transform fault zone and adjacent ridge segmentsPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1971
- I. Ultramafic rocks - Peridotite—gabbro—basalt complex from the equatorial Mid-Atlantic RidgePhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1971
- Layered Basic Complex in Oceanic Crust, Romanche Fracture, Equatorial Atlantic OceanScience, 1970
- The Mid-Atlantic Ridge near 45& deg;N. III. Bald MountainCanadian Journal of Earth Sciences, 1969
- The Mid-Atlantic Ridge near 45° N. II. Basalts from the area of Confederation PeakCanadian Journal of Earth Sciences, 1968
- North atlantic fracture zones near 53°Earth and Planetary Science Letters, 1967
- Chemical Characteristics of Oceanic Basalts and the Upper MantleGSA Bulletin, 1965
- Basalts from the deep ocean floorMineralogical Magazine and Journal of the Mineralogical Society, 1965