Synthesis of pyrope–grossular garnets: an experimental study at P = 2.5 GPa
Summary ¶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...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Orlando, A. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2003 |
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| Schlagwörter: |
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| Systematik: |
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| Anmerkung: |
© Springer-Verlag/Wien 2002 |
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| Übergeordnetes Werk: |
Enthalten in: Mineralogy and petrology - Springer-Verlag, 1987, 78(2003), 1 vom: Apr., Seite 37-51 |
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| Übergeordnetes Werk: |
volume:78 ; year:2003 ; number:1 ; month:04 ; pages:37-51 |
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| DOI / URN: |
10.1007/s00710-002-0223-2 |
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OLC2062483511 |
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| 520 | |a Summary ¶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. | ||
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10.1007/s00710-002-0223-2 doi (DE-627)OLC2062483511 (DE-He213)s00710-002-0223-2-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Orlando, A. verfasserin aut Synthesis of pyrope–grossular garnets: an experimental study at P = 2.5 GPa 2003 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag/Wien 2002 Summary ¶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. Experimental Study Crystalline Phase Middle Part Diopside Rich Side Borrini, D. aut Enthalten in Mineralogy and petrology Springer-Verlag, 1987 78(2003), 1 vom: Apr., Seite 37-51 (DE-627)129383856 (DE-600)166036-6 (DE-576)014770881 0930-0708 nnns volume:78 year:2003 number:1 month:04 pages:37-51 https://doi.org/10.1007/s00710-002-0223-2 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_2399 GBV_ILN_4112 GBV_ILN_4306 TE 1000 AR 78 2003 1 04 37-51 |
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synthesis of pyrope–grossular garnets: an experimental study at p = 2.5 gpa |
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Synthesis of pyrope–grossular garnets: an experimental study at P = 2.5 GPa |
| abstract |
Summary ¶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. © Springer-Verlag/Wien 2002 |
| abstractGer |
Summary ¶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. © Springer-Verlag/Wien 2002 |
| abstract_unstemmed |
Summary ¶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. © Springer-Verlag/Wien 2002 |
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| title_short |
Synthesis of pyrope–grossular garnets: an experimental study at P = 2.5 GPa |
| url |
https://doi.org/10.1007/s00710-002-0223-2 |
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Borrini, D. |
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| doi_str |
10.1007/s00710-002-0223-2 |
| up_date |
2024-07-03T15:14:23.960Z |
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