High-temperature behavior of quartz-in-garnet system revealed by in situ Raman spectroscopy
Abstract Quartz is one of the most abundant minerals in the Earth crust and therefore quartz inclusions in garnet are of great interest for elastic geobarometry, an approach that exploits the elastic properties of the mineral pair to back-calculate the conditions of inclusion entrapment. However, th...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Morana, Marta [verfasserIn] |
|---|
| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2023 |
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| Schlagwörter: |
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| Anmerkung: |
© The Author(s) 2023 |
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| Übergeordnetes Werk: |
Enthalten in: Physics and chemistry of minerals - Springer Berlin Heidelberg, 1977, 50(2023), 3 vom: 07. Juli |
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| Übergeordnetes Werk: |
volume:50 ; year:2023 ; number:3 ; day:07 ; month:07 |
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10.1007/s00269-023-01246-5 |
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OLC2144351244 |
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| 520 | |a Abstract Quartz is one of the most abundant minerals in the Earth crust and therefore quartz inclusions in garnet are of great interest for elastic geobarometry, an approach that exploits the elastic properties of the mineral pair to back-calculate the conditions of inclusion entrapment. However, the high-temperature behavior of quartz inclusions close to the $$\alpha$$–$$\beta$$ transition boundary has not been studied experimentally. We have therefore performed in situ high-temperature Raman spectroscopy on a quartz-in-garnet system up to 1000 K, and have also collected an improved reference data set for the temperature dependence of the Raman scattering of free quartz. Our results show that the $$\alpha$$-to-$$\beta$$ phase transition is hindered by the stress imposed by the host on the quartz inclusion, resulting in a thermosalient effect of the whole host-inclusion system or a mechanical cracking of the host mineral. | ||
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| 700 | 1 | |a Alvaro, Matteo |4 aut | |
| 700 | 1 | |a Mihailova, Boriana |4 aut | |
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10.1007/s00269-023-01246-5 doi (DE-627)OLC2144351244 (DE-He213)s00269-023-01246-5-p DE-627 ger DE-627 rakwb eng 550 540 530 VZ BIODIV DE-30 fid Morana, Marta verfasserin aut High-temperature behavior of quartz-in-garnet system revealed by in situ Raman spectroscopy 2023 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2023 Abstract Quartz is one of the most abundant minerals in the Earth crust and therefore quartz inclusions in garnet are of great interest for elastic geobarometry, an approach that exploits the elastic properties of the mineral pair to back-calculate the conditions of inclusion entrapment. However, the high-temperature behavior of quartz inclusions close to the $$\alpha$$–$$\beta$$ transition boundary has not been studied experimentally. We have therefore performed in situ high-temperature Raman spectroscopy on a quartz-in-garnet system up to 1000 K, and have also collected an improved reference data set for the temperature dependence of the Raman scattering of free quartz. Our results show that the $$\alpha$$-to-$$\beta$$ phase transition is hindered by the stress imposed by the host on the quartz inclusion, resulting in a thermosalient effect of the whole host-inclusion system or a mechanical cracking of the host mineral. Host-inclusion system Geobarometry Phase transition Thermoelastic properties Angel, Ross J. aut Alvaro, Matteo aut Mihailova, Boriana aut Enthalten in Physics and chemistry of minerals Springer Berlin Heidelberg, 1977 50(2023), 3 vom: 07. Juli (DE-627)129323039 (DE-600)131393-9 (DE-576)014557398 0342-1791 nnns volume:50 year:2023 number:3 day:07 month:07 https://doi.org/10.1007/s00269-023-01246-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-GEO SSG-OLC-PHA SSG-OPC-GGO GBV_ILN_32 GBV_ILN_2018 GBV_ILN_4277 AR 50 2023 3 07 07 |
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10.1007/s00269-023-01246-5 doi (DE-627)OLC2144351244 (DE-He213)s00269-023-01246-5-p DE-627 ger DE-627 rakwb eng 550 540 530 VZ BIODIV DE-30 fid Morana, Marta verfasserin aut High-temperature behavior of quartz-in-garnet system revealed by in situ Raman spectroscopy 2023 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2023 Abstract Quartz is one of the most abundant minerals in the Earth crust and therefore quartz inclusions in garnet are of great interest for elastic geobarometry, an approach that exploits the elastic properties of the mineral pair to back-calculate the conditions of inclusion entrapment. However, the high-temperature behavior of quartz inclusions close to the $$\alpha$$–$$\beta$$ transition boundary has not been studied experimentally. We have therefore performed in situ high-temperature Raman spectroscopy on a quartz-in-garnet system up to 1000 K, and have also collected an improved reference data set for the temperature dependence of the Raman scattering of free quartz. Our results show that the $$\alpha$$-to-$$\beta$$ phase transition is hindered by the stress imposed by the host on the quartz inclusion, resulting in a thermosalient effect of the whole host-inclusion system or a mechanical cracking of the host mineral. Host-inclusion system Geobarometry Phase transition Thermoelastic properties Angel, Ross J. aut Alvaro, Matteo aut Mihailova, Boriana aut Enthalten in Physics and chemistry of minerals Springer Berlin Heidelberg, 1977 50(2023), 3 vom: 07. Juli (DE-627)129323039 (DE-600)131393-9 (DE-576)014557398 0342-1791 nnns volume:50 year:2023 number:3 day:07 month:07 https://doi.org/10.1007/s00269-023-01246-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-GEO SSG-OLC-PHA SSG-OPC-GGO GBV_ILN_32 GBV_ILN_2018 GBV_ILN_4277 AR 50 2023 3 07 07 |
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10.1007/s00269-023-01246-5 doi (DE-627)OLC2144351244 (DE-He213)s00269-023-01246-5-p DE-627 ger DE-627 rakwb eng 550 540 530 VZ BIODIV DE-30 fid Morana, Marta verfasserin aut High-temperature behavior of quartz-in-garnet system revealed by in situ Raman spectroscopy 2023 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2023 Abstract Quartz is one of the most abundant minerals in the Earth crust and therefore quartz inclusions in garnet are of great interest for elastic geobarometry, an approach that exploits the elastic properties of the mineral pair to back-calculate the conditions of inclusion entrapment. However, the high-temperature behavior of quartz inclusions close to the $$\alpha$$–$$\beta$$ transition boundary has not been studied experimentally. We have therefore performed in situ high-temperature Raman spectroscopy on a quartz-in-garnet system up to 1000 K, and have also collected an improved reference data set for the temperature dependence of the Raman scattering of free quartz. Our results show that the $$\alpha$$-to-$$\beta$$ phase transition is hindered by the stress imposed by the host on the quartz inclusion, resulting in a thermosalient effect of the whole host-inclusion system or a mechanical cracking of the host mineral. Host-inclusion system Geobarometry Phase transition Thermoelastic properties Angel, Ross J. aut Alvaro, Matteo aut Mihailova, Boriana aut Enthalten in Physics and chemistry of minerals Springer Berlin Heidelberg, 1977 50(2023), 3 vom: 07. Juli (DE-627)129323039 (DE-600)131393-9 (DE-576)014557398 0342-1791 nnns volume:50 year:2023 number:3 day:07 month:07 https://doi.org/10.1007/s00269-023-01246-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-GEO SSG-OLC-PHA SSG-OPC-GGO GBV_ILN_32 GBV_ILN_2018 GBV_ILN_4277 AR 50 2023 3 07 07 |
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10.1007/s00269-023-01246-5 doi (DE-627)OLC2144351244 (DE-He213)s00269-023-01246-5-p DE-627 ger DE-627 rakwb eng 550 540 530 VZ BIODIV DE-30 fid Morana, Marta verfasserin aut High-temperature behavior of quartz-in-garnet system revealed by in situ Raman spectroscopy 2023 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2023 Abstract Quartz is one of the most abundant minerals in the Earth crust and therefore quartz inclusions in garnet are of great interest for elastic geobarometry, an approach that exploits the elastic properties of the mineral pair to back-calculate the conditions of inclusion entrapment. However, the high-temperature behavior of quartz inclusions close to the $$\alpha$$–$$\beta$$ transition boundary has not been studied experimentally. We have therefore performed in situ high-temperature Raman spectroscopy on a quartz-in-garnet system up to 1000 K, and have also collected an improved reference data set for the temperature dependence of the Raman scattering of free quartz. Our results show that the $$\alpha$$-to-$$\beta$$ phase transition is hindered by the stress imposed by the host on the quartz inclusion, resulting in a thermosalient effect of the whole host-inclusion system or a mechanical cracking of the host mineral. Host-inclusion system Geobarometry Phase transition Thermoelastic properties Angel, Ross J. aut Alvaro, Matteo aut Mihailova, Boriana aut Enthalten in Physics and chemistry of minerals Springer Berlin Heidelberg, 1977 50(2023), 3 vom: 07. Juli (DE-627)129323039 (DE-600)131393-9 (DE-576)014557398 0342-1791 nnns volume:50 year:2023 number:3 day:07 month:07 https://doi.org/10.1007/s00269-023-01246-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-GEO SSG-OLC-PHA SSG-OPC-GGO GBV_ILN_32 GBV_ILN_2018 GBV_ILN_4277 AR 50 2023 3 07 07 |
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10.1007/s00269-023-01246-5 doi (DE-627)OLC2144351244 (DE-He213)s00269-023-01246-5-p DE-627 ger DE-627 rakwb eng 550 540 530 VZ BIODIV DE-30 fid Morana, Marta verfasserin aut High-temperature behavior of quartz-in-garnet system revealed by in situ Raman spectroscopy 2023 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2023 Abstract Quartz is one of the most abundant minerals in the Earth crust and therefore quartz inclusions in garnet are of great interest for elastic geobarometry, an approach that exploits the elastic properties of the mineral pair to back-calculate the conditions of inclusion entrapment. However, the high-temperature behavior of quartz inclusions close to the $$\alpha$$–$$\beta$$ transition boundary has not been studied experimentally. We have therefore performed in situ high-temperature Raman spectroscopy on a quartz-in-garnet system up to 1000 K, and have also collected an improved reference data set for the temperature dependence of the Raman scattering of free quartz. Our results show that the $$\alpha$$-to-$$\beta$$ phase transition is hindered by the stress imposed by the host on the quartz inclusion, resulting in a thermosalient effect of the whole host-inclusion system or a mechanical cracking of the host mineral. Host-inclusion system Geobarometry Phase transition Thermoelastic properties Angel, Ross J. aut Alvaro, Matteo aut Mihailova, Boriana aut Enthalten in Physics and chemistry of minerals Springer Berlin Heidelberg, 1977 50(2023), 3 vom: 07. Juli (DE-627)129323039 (DE-600)131393-9 (DE-576)014557398 0342-1791 nnns volume:50 year:2023 number:3 day:07 month:07 https://doi.org/10.1007/s00269-023-01246-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-PHY SSG-OLC-CHE SSG-OLC-GEO SSG-OLC-PHA SSG-OPC-GGO GBV_ILN_32 GBV_ILN_2018 GBV_ILN_4277 AR 50 2023 3 07 07 |
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high-temperature behavior of quartz-in-garnet system revealed by in situ raman spectroscopy |
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High-temperature behavior of quartz-in-garnet system revealed by in situ Raman spectroscopy |
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Abstract Quartz is one of the most abundant minerals in the Earth crust and therefore quartz inclusions in garnet are of great interest for elastic geobarometry, an approach that exploits the elastic properties of the mineral pair to back-calculate the conditions of inclusion entrapment. However, the high-temperature behavior of quartz inclusions close to the $$\alpha$$–$$\beta$$ transition boundary has not been studied experimentally. We have therefore performed in situ high-temperature Raman spectroscopy on a quartz-in-garnet system up to 1000 K, and have also collected an improved reference data set for the temperature dependence of the Raman scattering of free quartz. Our results show that the $$\alpha$$-to-$$\beta$$ phase transition is hindered by the stress imposed by the host on the quartz inclusion, resulting in a thermosalient effect of the whole host-inclusion system or a mechanical cracking of the host mineral. © The Author(s) 2023 |
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Abstract Quartz is one of the most abundant minerals in the Earth crust and therefore quartz inclusions in garnet are of great interest for elastic geobarometry, an approach that exploits the elastic properties of the mineral pair to back-calculate the conditions of inclusion entrapment. However, the high-temperature behavior of quartz inclusions close to the $$\alpha$$–$$\beta$$ transition boundary has not been studied experimentally. We have therefore performed in situ high-temperature Raman spectroscopy on a quartz-in-garnet system up to 1000 K, and have also collected an improved reference data set for the temperature dependence of the Raman scattering of free quartz. Our results show that the $$\alpha$$-to-$$\beta$$ phase transition is hindered by the stress imposed by the host on the quartz inclusion, resulting in a thermosalient effect of the whole host-inclusion system or a mechanical cracking of the host mineral. © The Author(s) 2023 |
| abstract_unstemmed |
Abstract Quartz is one of the most abundant minerals in the Earth crust and therefore quartz inclusions in garnet are of great interest for elastic geobarometry, an approach that exploits the elastic properties of the mineral pair to back-calculate the conditions of inclusion entrapment. However, the high-temperature behavior of quartz inclusions close to the $$\alpha$$–$$\beta$$ transition boundary has not been studied experimentally. We have therefore performed in situ high-temperature Raman spectroscopy on a quartz-in-garnet system up to 1000 K, and have also collected an improved reference data set for the temperature dependence of the Raman scattering of free quartz. Our results show that the $$\alpha$$-to-$$\beta$$ phase transition is hindered by the stress imposed by the host on the quartz inclusion, resulting in a thermosalient effect of the whole host-inclusion system or a mechanical cracking of the host mineral. © The Author(s) 2023 |
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| title_short |
High-temperature behavior of quartz-in-garnet system revealed by in situ Raman spectroscopy |
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https://doi.org/10.1007/s00269-023-01246-5 |
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Angel, Ross J. Alvaro, Matteo Mihailova, Boriana |
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10.1007/s00269-023-01246-5 |
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2024-07-03T21:40:36.393Z |
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