SYNTHESIS OF PYROPE-GROSSULAR GARNETS: AN EXPERIMENTAL STUDY AT P = 2.5 GPA
- DSpace Home
- →
- Геология России
- →
- ELibrary
- →
- View Item
JavaScript is disabled for your browser. Some features of this site may not work without it.
dc.contributor.author | Orlando A. | |
dc.contributor.author | Borrini D. | |
dc.date.accessioned | 2021-12-30T03:20:45Z | |
dc.date.available | 2021-12-30T03:20:45Z | |
dc.date.issued | 2003 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=5089451 | |
dc.identifier.citation | Mineralogy and Petrology, 2003, 78, 1-2, 37-51 | |
dc.identifier.issn | 0930-0708 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/33946 | |
dc.description.abstract | In order to evaluate the stability of Mg-Ca garnets at P = 2.5 GPa/T = 800-1500 °C, some experiments were performed using both natural and synthetic starting materials. Particular attention was paid to the investigation of the Ca rich side of the pyrope-grossular join and the maximum pyrope content in grossular was found to be about 10 mol.%. The addition of Cr to the system only slightly increases the observed pyrope solubility in grossular whereas Na stabilises melilite and merwinite. Clinopyroxene with a composition lying on the diopside - Ca Tschermak join appears to be the only stable crystalline phase in the middle part of the pyrope-grossular join. | |
dc.title | SYNTHESIS OF PYROPE-GROSSULAR GARNETS: AN EXPERIMENTAL STUDY AT P = 2.5 GPA | |
dc.type | Статья |
Files in this item
This item appears in the following Collection(s)
-
ELibrary
Метаданные публикаций с сайта https://www.elibrary.ru