Evolution of the ‘FAMOUS’ Ocean Ridge Segment: Evidence from submarine and deep sea drilling investigations
Author:
Publisher
American Geophysical Union
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1029/ME002p0314/fullpdf
Reference42 articles.
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2. Emplacement models of ocean crust: constraints from FAMOUS area data (abstract);Atwater,1978
3. Initial Reports of the Deep Sea Drilling Project;Aumento,1977
4. Morphology and tectonics of the inner rift valley at lat. 36° 50′N. on the Mid-Atlantic Ridge;Ballard;Geol. Soc. Amer. Bull.,1977
5. Current rifting episode in northern Iceland;Björnsson;Nature,1978
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1. Steady and non-steady state magma chambers below the East Pacific Rise;Geophysical Research Letters;1996-02-01
2. The significance of unusual zoning in olivines from FAMOUS area basalt 527-1-1;Contributions to Mineralogy and Petrology;1986
3. The volcanic-tectonic cycle of the FAMOUS and AMAR Valleys, Mid-Atlantic Ridge (36°47′N): Evidence from basalt glass and phenocryst compositional variations for a steady state magma chamber beneath the valley midsections, AMAR 3;Journal of Geophysical Research: Solid Earth;1984-08-10
4. Systematics of modal phenocryst assemblages in submarine basalts: Petrologic implications;Contributions to Mineralogy and Petrology;1983-08
5. Thermal and kinematic control on ocean-ridge magma fractionation: contrasts between Atlantic and Pacific spreading axes;Journal of the Geological Society;1981-11
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