Magma chambers in the Oman ophiolite: fed from the top and the bottom
- 1 October 1996
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 144 (1-2) , 239-250
- https://doi.org/10.1016/0012-821x(96)00167-7
Abstract
No abstract availableKeywords
This publication has 26 references indexed in Scilit:
- Duality of magmatism in the plutonic sequence of the Sumail Nappe, OmanPublished by Elsevier ,2003
- A new magma chamber model based on structural studies in the Oman ophiolitePublished by Elsevier ,2003
- Variability in oceanic crustal thickness and structure: Multichannel seismic reflection results from the northern East Pacific RiseJournal of Geophysical Research, 1996
- Flow mechanism and viscosity in basaltic magma chambersGeophysical Research Letters, 1996
- Mapping oceanic ridge segments in Oman ophioliteJournal of Geophysical Research, 1995
- Evidence from the Oman ophiolite for active mantle upwelling beneath a fast-spreading ridgeNature, 1994
- Oceanic crust as a reactive filter: Synkinematic intrusion, hybridization, and assimilation in an ophiolitic magma chamber, western NewfoundlandGeology, 1993
- Magma chambers at oceanic ridges: How large?Geology, 1993
- Mantle—crust transition zone and origin of wehrlitic magmas: Evidence from the Oman ophioliteTectonophysics, 1988
- Deformation-Induced Recrystallization Due to Progressive Misorientation of Subgrains, with Special Reference to Mantle PeridotitesThe Journal of Geology, 1975