Petrology of a chromitite micropod from Hess Deep, equatorial Pacific: a comparison between abyssal and alpine-type podiform chromitites
Authors:
- Shoji AraiSAShoji Arai
Abstract
No abstract availableKeywords
This publication has 42 references indexed in Scilit:
- Hydrous mineral inclusions in chromian spinel from the Yanomine ultramafic complex of the Sangun zone, Southwest Japan.JOURNAL OF MINERALOGY, PETROLOGY AND ECONOMIC GEOLOGY, 1995
- Characterization of spinel peridotites by olivine-spinel compositional relationships: Review and interpretationChemical Geology, 1994
- Compositional variation of olivine-chromian spinel in Mg-rich magmas as a guide to their residual spinel peridotitesJournal of Volcanology and Geothermal Research, 1994
- Plagioclase-wehrlites and peridotites on the East Pacific Rise (Hess Deep) and the Mid-Atlantic Ridge (DSDP Site 334): evidence for magma percolation in the oceanic upper mantleEarth and Planetary Science Letters, 1993
- Dyke complex of the East Pacific Rise exposed in the walls of Hess Deep and the structure of the upper oceanic crustEarth and Planetary Science Letters, 1992
- 1 Ma East Pacific Rise oceanic crust and uppermost mantle exposed by rifting in Hess Deep (equatorial Pacific Ocean)Earth and Planetary Science Letters, 1990
- Characteristics and tectonic significance of supra-subduction zone ophiolitesGeological Society, London, Special Publications, 1984
- Ultramafic and mafic rocks from the Garret Transform Fault near 13°30′S on the East Pacific Rise: Igneous petrologyEarth and Planetary Science Letters, 1983
- Platinum-group minerals and other solid inclusions in chromite of ophiolitic complexes: Occurrence and petrological significanceMineralogy and Petrology, 1983
- CHROMIAN SPINEL AS A PETROGENETIC INDICATOR: PART 1. THEORYCanadian Journal of Earth Sciences, 1965