Constraining the cooling rate of the lower oceanic crust: a new approach applied to the Oman ophiolite
- 29 March 2002
- journal article
- Published by Elsevier
- Vol. 199 (1-2) , 127-146
- https://doi.org/10.1016/s0012-821x(02)00554-x
Abstract
No abstract availableKeywords
This publication has 55 references indexed in Scilit:
- Shear zones, thrusts and related magmatism in the Oman ophiolite: Initiation of thrusting on an oceanic ridgePublished by Elsevier ,2003
- Duality of magmatism in the plutonic sequence of the Sumail Nappe, OmanPublished by Elsevier ,2003
- Variation of cooling rate with depth in lower crust formed at an oceanic spreading ridge: Plagioclase crystal size distributions in gabbros from the Oman ophioliteGeochemistry, Geophysics, Geosystems, 2001
- Thermal effects of gabbro accretion from a deeper second melt lens at the fast spreading East Pacific RiseJournal of Geophysical Research, 2001
- A fossil melt lens in the Oman ophiolite: Implications for magma chamber processes at fast spreading ridgesEarth and Planetary Science Letters, 2000
- Chemical zoning of olivine in several pallasitesJournal of Geophysical Research, 1997
- The effects of spreading rate, the magma budget, and the geometry of magma emplacement on the axial heat flux at mid‐ocean ridgesJournal of Geophysical Research, 1996
- Mapping oceanic ridge segments in Oman ophioliteJournal of Geophysical Research, 1995
- Magnesium grain boundary diffusion in forsterite aggregates at 1000°–1300°C and 0.1 MPa to 10 GPaJournal of Geophysical Research, 1994
- Flow porosities, permeabilities and preliminary data on fluid inclusions and fossil thermal gradients in the crustal sequence of the Sumail ophiolite (Oman)Tectonophysics, 1988