Mantle—crust transition zone and origin of wehrlitic magmas: Evidence from the Oman ophiolite
- 1 September 1988
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 151 (1-4) , 75-85
- https://doi.org/10.1016/0040-1951(88)90241-7
Abstract
No abstract availableKeywords
This publication has 22 references indexed in Scilit:
- Geochemistry and petrogenesis of the Lanzo peridotite body, western AlpsTectonophysics, 1988
- Natural deformation fabrics of plagioclase: implications for slip systems and seismic anisotropyTectonophysics, 1988
- Structure and petrology of peridotites: Clues to their geodynamic environmentReviews of Geophysics, 1986
- Cumulative or Residual Origin for the Transition Zone in Ophiolites: Structural EvidenceJournal of Petrology, 1983
- Terminology for Layered IntrusionsJournal of Petrology, 1982
- Mantle flow at oceanic spreading centers: Models derived from ophiolitesTectonophysics, 1982
- Structural petrology of the Olympus ultramafic complex in the Troodos ophiolite, CyprusGSA Bulletin, 1978
- Equilibration History of the Basel Alpine-Type Peridotite, Red Mountain, New ZealandJournal of Petrology, 1977
- New Model for the Structure of the Ocean CrustNature, 1970
- Origin of ultramafic rocks, their tectonic setting and history: A contribution to the discussion of the paper “the origin of ultramafic and ultrabasic rocks” by P.J. WyllieTectonophysics, 1969