Na and Cr contents in clinopyroxenes from peridotites: A possible discriminant between “sub-continental” and “sub-oceanic” mantle
- 1 April 1981
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 53 (2) , 241-254
- https://doi.org/10.1016/0012-821x(81)90157-6
Abstract
No abstract availableKeywords
This publication has 57 references indexed in Scilit:
- Ocean-continent boundary off the Iberian margin: A serpentinite diapir west of the Galicia BankEarth and Planetary Science Letters, 1980
- Experimental study on the phase equilibria in the join CaMgSi2O6-CaCrCrSiO6 with special reference to the blue diopsideContributions to Mineralogy and Petrology, 1977
- Serpentinite protrusions in the oceanic crustEarth and Planetary Science Letters, 1976
- The system diopside-ureyite at 20 KbContributions to Mineralogy and Petrology, 1975
- Homologies geologiques entre les deux rives du detroit de GibraltarBSGF - Earth Sciences Bulletin, 1973
- Synthesis of kosmochlor and phase equilibria in the join CaMgSi2O6-NaCrSi2O6Contributions to Mineralogy and Petrology, 1972
- Petrology of a transform fault zone and adjacent ridge segmentsPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1971
- I. Ultramafic rocks - Peridotite—gabbro—basalt complex from the equatorial Mid-Atlantic RidgePhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1971
- Mountain belts and the new global tectonicsJournal of Geophysical Research, 1970
- Sind die alpinotypen Peridotitmassen vielleicht tektonisch verfrachtete Bruchstücke der Peridotitschale?International Journal of Earth Sciences, 1957