Geochemical effects of dynamic melting beneath ridges: Reconciling major and trace element variations in Kolbeinsey (and global) mid‐ocean ridge basalt
- 10 May 1994
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 99 (B5) , 9077-9095
- https://doi.org/10.1029/93jb03364
Abstract
No abstract availableKeywords
This publication has 35 references indexed in Scilit:
- Sr-Nd-Pb isotope evidence against plume-asthenosphere mixing north of IcelandPublished by Elsevier ,2002
- Some remarks on the movement of small melt fractions in the mantlePublished by Elsevier ,2002
- Geochemical consequences of in situ crystallizationNature, 1989
- Chemical differentiation of the Earth: the relationship between mantle, continental crust, and oceanic crustEarth and Planetary Science Letters, 1988
- Geochemistry of basalts from the Indian Ocean triple junction: implications for the generation and evolution of Indian Ocean ridge basaltsEarth and Planetary Science Letters, 1986
- Magmagenesis and the mapping of chemical and isotopic variations in the mantleChemical Geology, 1986
- An assessment of the relative roles of crust and mantle in magma genesis: an elemental approachPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1984
- Melting relations of a magnesian abyssal tholeiite and the origin of MORBsEarth and Planetary Science Letters, 1983
- Nickel partitioning between olivine and silicate meltEarth and Planetary Science Letters, 1978
- Evolution of the Axial Rifting Zone in Northern Iceland and the Tjörnes Fracture ZoneGSA Bulletin, 1974