Na, K, P and Ti in garnet, pyroxene and olivine from peridotite and eclogite xenoliths from African kimberlites
- 4 April 1978
- Vol. 11 (2), 155-173
- https://doi.org/10.1016/0024-4937(78)90006-3
Abstract
No abstract availableKeywords
This publication has 48 references indexed in Scilit:
- Diopside-enstatite equilibria at 850 degrees to 1400 degrees C, 5 to 35 kbAmerican Journal of Science, 1976
- Statistical Classification of Garnets from Kimberlite and Associated Xenoliths: AddendumThe Journal of Geology, 1976
- Determination of the P,T paths of natural eclogites during metamorphism—record of subductionLithos, 1976
- Na, P, Ti and coordination of Si in garnet from peridotite and eclogite xenolithsNature, 1976
- Pyroxenes in the system Mg2Si2O6-CaMgSi2O6 at high pressureEarth and Planetary Science Letters, 1975
- Is upper-mantle phosphorus contained in sodic garnet?Earth and Planetary Science Letters, 1975
- Occurrence of diamond in a mica–garnet Iherzolite xenolith from kimberliteNature, 1975
- Potassium contents of synthetic clinopyroxenes at high pressures and temperaturesEarth and Planetary Science Letters, 1971
- Rb/K ratios and Sr-isotopic compositions of minerals in eclogitic and peridotitic rocksEarth and Planetary Science Letters, 1968
- X-Ray-Emission Microanalysis of Rock-Forming Minerals II. OlivinesThe Journal of Geology, 1966