Crustal diopsidites from the northern Oman ophiolite: Evidence for hydrothermal circulation through suboceanic Moho
Author:
Publisher
Japan Association of Mineralogical Sciences
Subject
Geology,Geophysics
Reference27 articles.
1. Abily, B., Ceuleneer, G. and Launeau, P. (2011) Synmagmatic normal faulting in the lower oceanic crust: Evidence from the Oman ophiolite. Geology, 39, 391-394.
2. Akizawa, N. and Arai, S. (2009) Petrologic profile of a peridotite layer under a possible Moho in the northern Oman ophiolite: an example from Wadi Fizh. Journal of Mineralogical and Petrological Societies, 104, 389-394.
3. Deep and High-temperature Hydrothermal Circulation in the Oman Ophiolite--Petrological and Isotopic Evidence
4. Dick, H.J.B. and Natland, J.H. (1996) Late-stage melt evolution and transport in the shallow mantle beneath the East Pacific Rise. Proceedings of the Ocean Drilling Program, Scientific Results, 147, 103-134.
5. Origin of high-Al N-MORB by fractional crystallization in the upper mantle beneath the Galápagos Spreading Center
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