Geochemistry of gabbro sills in the crust-mantle transition zone of the Oman ophiolite: implications for the origin of the oceanic lower crust
- 1 February 1997
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 146 (3-4) , 475-488
- https://doi.org/10.1016/s0012-821x(96)00235-x
Abstract
No abstract availableKeywords
This publication has 58 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
- Emplacement of dikes, sills and crustal magma chambers at divergent plate boundariesPublished by Elsevier ,2003
- Flow mechanism and viscosity in basaltic magma chambersGeophysical Research Letters, 1996
- Experiments on flow focusing in soluble porous media, with applications to melt extraction from the mantleJournal of Geophysical Research, 1995
- Magma chambers at oceanic ridges: How large?Geology, 1993
- The death of an accretion zone as evidenced by the magmatic history of the Sumail ophiolite (Oman)Tectonophysics, 1988
- Segmentation at a fossil spreading axis: The plutonic sequence of the Wadi Haymiliyah area (Haylayn Block, Sumail Nappe, Oman)Tectonophysics, 1988
- Complexity of the crustal sequence in the northern Oman ophiolite (Fizh and southern Aswad blocks): The effect of early slicing?Tectonophysics, 1988
- Mantle—crust transition zone and origin of wehrlitic magmas: Evidence from the Oman ophioliteTectonophysics, 1988