The PT-phase relations of an MgO-rich Hawaiian tholeiite: the compositions of primary Hawaiian tholeiites
Abstract The PT-phase relations of a Hawaiian tholeiite with 18.2% MgO has olivine–orthopyroxene multiple saturation at 20.5 kbar and 1,550°C. This pressure is less than the pressure at the lithosphere/asthenosphere transition, and it is suggested that tholeiites with this and lesser MgO contents ar...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Maaløe, S. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2004 |
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| Schlagwörter: |
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| Systematik: |
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| Anmerkung: |
© Springer-Verlag 2004 |
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| Übergeordnetes Werk: |
Enthalten in: Contributions to mineralogy and petrology - Springer-Verlag, 1966, 148(2004), 2 vom: 07. Sept., Seite 236-246 |
|---|---|
| Übergeordnetes Werk: |
volume:148 ; year:2004 ; number:2 ; day:07 ; month:09 ; pages:236-246 |
| Links: |
|---|
| DOI / URN: |
10.1007/s00410-004-0601-3 |
|---|
| Katalog-ID: |
OLC2070524159 |
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| 520 | |a Abstract The PT-phase relations of a Hawaiian tholeiite with 18.2% MgO has olivine–orthopyroxene multiple saturation at 20.5 kbar and 1,550°C. This pressure is less than the pressure at the lithosphere/asthenosphere transition, and it is suggested that tholeiites with this and lesser MgO contents are fractionated. Assuming a harzburgitic residuum it is shown that Hawaiian primary tholeiites contain about 23% MgO, and are generated at 36±5 kbar and 1,680±50°C. This pressure is equivalent to a depth of 112 km, which is consistent with the thickness of the lithosphere and thermal plume modeling. The minimal MgO content of primary Hawaiian tholeiites is suggested as 19% MgO. | ||
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10.1007/s00410-004-0601-3 doi (DE-627)OLC2070524159 (DE-He213)s00410-004-0601-3-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Maaløe, S. verfasserin aut The PT-phase relations of an MgO-rich Hawaiian tholeiite: the compositions of primary Hawaiian tholeiites 2004 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2004 Abstract The PT-phase relations of a Hawaiian tholeiite with 18.2% MgO has olivine–orthopyroxene multiple saturation at 20.5 kbar and 1,550°C. This pressure is less than the pressure at the lithosphere/asthenosphere transition, and it is suggested that tholeiites with this and lesser MgO contents are fractionated. Assuming a harzburgitic residuum it is shown that Hawaiian primary tholeiites contain about 23% MgO, and are generated at 36±5 kbar and 1,680±50°C. This pressure is equivalent to a depth of 112 km, which is consistent with the thickness of the lithosphere and thermal plume modeling. The minimal MgO content of primary Hawaiian tholeiites is suggested as 19% MgO. Olivine Lithosphere Primary Magma Olivine Phenocryst Primary Composition Enthalten in Contributions to mineralogy and petrology Springer-Verlag, 1966 148(2004), 2 vom: 07. Sept., Seite 236-246 (DE-627)129068721 (DE-600)1616-0 (DE-576)014400367 0010-7999 nnns volume:148 year:2004 number:2 day:07 month:09 pages:236-246 https://doi.org/10.1007/s00410-004-0601-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_70 GBV_ILN_285 GBV_ILN_381 GBV_ILN_2004 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4112 GBV_ILN_4277 GBV_ILN_4306 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4323 TE 1000 AR 148 2004 2 07 09 236-246 |
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10.1007/s00410-004-0601-3 doi (DE-627)OLC2070524159 (DE-He213)s00410-004-0601-3-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Maaløe, S. verfasserin aut The PT-phase relations of an MgO-rich Hawaiian tholeiite: the compositions of primary Hawaiian tholeiites 2004 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2004 Abstract The PT-phase relations of a Hawaiian tholeiite with 18.2% MgO has olivine–orthopyroxene multiple saturation at 20.5 kbar and 1,550°C. This pressure is less than the pressure at the lithosphere/asthenosphere transition, and it is suggested that tholeiites with this and lesser MgO contents are fractionated. Assuming a harzburgitic residuum it is shown that Hawaiian primary tholeiites contain about 23% MgO, and are generated at 36±5 kbar and 1,680±50°C. This pressure is equivalent to a depth of 112 km, which is consistent with the thickness of the lithosphere and thermal plume modeling. The minimal MgO content of primary Hawaiian tholeiites is suggested as 19% MgO. Olivine Lithosphere Primary Magma Olivine Phenocryst Primary Composition Enthalten in Contributions to mineralogy and petrology Springer-Verlag, 1966 148(2004), 2 vom: 07. Sept., Seite 236-246 (DE-627)129068721 (DE-600)1616-0 (DE-576)014400367 0010-7999 nnns volume:148 year:2004 number:2 day:07 month:09 pages:236-246 https://doi.org/10.1007/s00410-004-0601-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_70 GBV_ILN_285 GBV_ILN_381 GBV_ILN_2004 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4112 GBV_ILN_4277 GBV_ILN_4306 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4323 TE 1000 AR 148 2004 2 07 09 236-246 |
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10.1007/s00410-004-0601-3 doi (DE-627)OLC2070524159 (DE-He213)s00410-004-0601-3-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Maaløe, S. verfasserin aut The PT-phase relations of an MgO-rich Hawaiian tholeiite: the compositions of primary Hawaiian tholeiites 2004 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2004 Abstract The PT-phase relations of a Hawaiian tholeiite with 18.2% MgO has olivine–orthopyroxene multiple saturation at 20.5 kbar and 1,550°C. This pressure is less than the pressure at the lithosphere/asthenosphere transition, and it is suggested that tholeiites with this and lesser MgO contents are fractionated. Assuming a harzburgitic residuum it is shown that Hawaiian primary tholeiites contain about 23% MgO, and are generated at 36±5 kbar and 1,680±50°C. This pressure is equivalent to a depth of 112 km, which is consistent with the thickness of the lithosphere and thermal plume modeling. The minimal MgO content of primary Hawaiian tholeiites is suggested as 19% MgO. Olivine Lithosphere Primary Magma Olivine Phenocryst Primary Composition Enthalten in Contributions to mineralogy and petrology Springer-Verlag, 1966 148(2004), 2 vom: 07. Sept., Seite 236-246 (DE-627)129068721 (DE-600)1616-0 (DE-576)014400367 0010-7999 nnns volume:148 year:2004 number:2 day:07 month:09 pages:236-246 https://doi.org/10.1007/s00410-004-0601-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_70 GBV_ILN_285 GBV_ILN_381 GBV_ILN_2004 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4112 GBV_ILN_4277 GBV_ILN_4306 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4323 TE 1000 AR 148 2004 2 07 09 236-246 |
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The PT-phase relations of an MgO-rich Hawaiian tholeiite: the compositions of primary Hawaiian tholeiites |
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The PT-phase relations of an MgO-rich Hawaiian tholeiite: the compositions of primary Hawaiian tholeiites |
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Maaløe, S. |
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Contributions to mineralogy and petrology |
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the pt-phase relations of an mgo-rich hawaiian tholeiite: the compositions of primary hawaiian tholeiites |
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The PT-phase relations of an MgO-rich Hawaiian tholeiite: the compositions of primary Hawaiian tholeiites |
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Abstract The PT-phase relations of a Hawaiian tholeiite with 18.2% MgO has olivine–orthopyroxene multiple saturation at 20.5 kbar and 1,550°C. This pressure is less than the pressure at the lithosphere/asthenosphere transition, and it is suggested that tholeiites with this and lesser MgO contents are fractionated. Assuming a harzburgitic residuum it is shown that Hawaiian primary tholeiites contain about 23% MgO, and are generated at 36±5 kbar and 1,680±50°C. This pressure is equivalent to a depth of 112 km, which is consistent with the thickness of the lithosphere and thermal plume modeling. The minimal MgO content of primary Hawaiian tholeiites is suggested as 19% MgO. © Springer-Verlag 2004 |
| abstractGer |
Abstract The PT-phase relations of a Hawaiian tholeiite with 18.2% MgO has olivine–orthopyroxene multiple saturation at 20.5 kbar and 1,550°C. This pressure is less than the pressure at the lithosphere/asthenosphere transition, and it is suggested that tholeiites with this and lesser MgO contents are fractionated. Assuming a harzburgitic residuum it is shown that Hawaiian primary tholeiites contain about 23% MgO, and are generated at 36±5 kbar and 1,680±50°C. This pressure is equivalent to a depth of 112 km, which is consistent with the thickness of the lithosphere and thermal plume modeling. The minimal MgO content of primary Hawaiian tholeiites is suggested as 19% MgO. © Springer-Verlag 2004 |
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Abstract The PT-phase relations of a Hawaiian tholeiite with 18.2% MgO has olivine–orthopyroxene multiple saturation at 20.5 kbar and 1,550°C. This pressure is less than the pressure at the lithosphere/asthenosphere transition, and it is suggested that tholeiites with this and lesser MgO contents are fractionated. Assuming a harzburgitic residuum it is shown that Hawaiian primary tholeiites contain about 23% MgO, and are generated at 36±5 kbar and 1,680±50°C. This pressure is equivalent to a depth of 112 km, which is consistent with the thickness of the lithosphere and thermal plume modeling. The minimal MgO content of primary Hawaiian tholeiites is suggested as 19% MgO. © Springer-Verlag 2004 |
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The PT-phase relations of an MgO-rich Hawaiian tholeiite: the compositions of primary Hawaiian tholeiites |
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