Constraints on the accretion of the gabbroic lower oceanic crust from plagioclase lattice preferred orientation in the Samail ophiolite

Author:

VanTongeren J.A.,Hirth G.,Kelemen P.B.

Funder

NSF-EAR

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference59 articles.

1. Preferred mineral orientations related to magmatic flow in ophiolite layered gabbros;Benn;J. Petrol.,1989

2. Deep and high-temperature hydrothermal circulation in the Oman ophiolite – petrological and isotopic evidence;Bosch;J. Petrol.,2004

3. Axial melt lenses at oceanic ridges – a case study in the Oman ophiolite;Boudier;Earth Planet. Sci. Lett.,2011

4. Magma chambers in the Oman ophiolite: fed from the top and the bottom;Boudier;Earth Planet. Sci. Lett.,1996

5. Cryptic variation within the cumulate sequence of the Oman ophiolite: magma chamber depth and petrological implications;Browning,1984

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