Mineralogy and partial melt textures within an ultramafic-mafic body, Greece
Abstract Ultramafic-mafic rocks from Makrirrakhi, Central Greece exhibit features of an original ophiolite sequence which contains depleted mantle material, ultramafic containing partial melt textures and possibly the mafic “pluton” which resulted from the coalescing of these partial melt segregatio...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Menzies, Martin [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
1973 |
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| Schlagwörter: |
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| Systematik: |
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| Anmerkung: |
© Springer-Verlag 1973 |
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| Übergeordnetes Werk: |
Enthalten in: Contributions to mineralogy and petrology - Springer-Verlag, 1966, 42(1973), 4 vom: Dez., Seite 273-285 |
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| Übergeordnetes Werk: |
volume:42 ; year:1973 ; number:4 ; month:12 ; pages:273-285 |
| Links: |
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| DOI / URN: |
10.1007/BF00372606 |
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| Katalog-ID: |
OLC2070485714 |
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| 245 | 1 | 0 | |a Mineralogy and partial melt textures within an ultramafic-mafic body, Greece |
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| 520 | |a Abstract Ultramafic-mafic rocks from Makrirrakhi, Central Greece exhibit features of an original ophiolite sequence which contains depleted mantle material, ultramafic containing partial melt textures and possibly the mafic “pluton” which resulted from the coalescing of these partial melt segregations. Considerable mineralogical variation exists: unzoned olivine crystals range in composition from $ Fo_{78–84} $ (mafics) to $ Fo_{88–92} $ (ultramafics), plagioclases $ An_{64–79} $ (mafics) to $ An_{80–90} $ (ultramafics) and spinel varies from a chromian spinel (ultramafics) to a more aluminous-titaniferous spinel (mafics). Pyroxenes from the ultramafics display a limited range: $ En_{89–92} $ $ Fs_{9–8} $ $ Wo_{0–2} $ (orthopyroxene) and $ En_{48–54} $ $ Fs_{1–10} $ $ Wo_{38–50} $ (clinopyroxene). Mafic rocks display a greater range being richer in ferrosilite $ En_{36–65} $ $ Fs_{3–20} $ $ Wo_{33–51} $. Pyroxenes from within the partial melt segregations have chemical affinities with those from the gabbrotroctolite series. A model of partial melt within the upper mantle, and, a set of criteria to distinguish partial melt textures from cumulate textures, are developed from analytical data and textural evidence. | ||
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10.1007/BF00372606 doi (DE-627)OLC2070485714 (DE-He213)BF00372606-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Menzies, Martin verfasserin aut Mineralogy and partial melt textures within an ultramafic-mafic body, Greece 1973 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1973 Abstract Ultramafic-mafic rocks from Makrirrakhi, Central Greece exhibit features of an original ophiolite sequence which contains depleted mantle material, ultramafic containing partial melt textures and possibly the mafic “pluton” which resulted from the coalescing of these partial melt segregations. Considerable mineralogical variation exists: unzoned olivine crystals range in composition from $ Fo_{78–84} $ (mafics) to $ Fo_{88–92} $ (ultramafics), plagioclases $ An_{64–79} $ (mafics) to $ An_{80–90} $ (ultramafics) and spinel varies from a chromian spinel (ultramafics) to a more aluminous-titaniferous spinel (mafics). Pyroxenes from the ultramafics display a limited range: $ En_{89–92} $ $ Fs_{9–8} $ $ Wo_{0–2} $ (orthopyroxene) and $ En_{48–54} $ $ Fs_{1–10} $ $ Wo_{38–50} $ (clinopyroxene). Mafic rocks display a greater range being richer in ferrosilite $ En_{36–65} $ $ Fs_{3–20} $ $ Wo_{33–51} $. Pyroxenes from within the partial melt segregations have chemical affinities with those from the gabbrotroctolite series. A model of partial melt within the upper mantle, and, a set of criteria to distinguish partial melt textures from cumulate textures, are developed from analytical data and textural evidence. Analytical Data Olivine Mineral Resource Limited Range Great Range Enthalten in Contributions to mineralogy and petrology Springer-Verlag, 1966 42(1973), 4 vom: Dez., Seite 273-285 (DE-627)129068721 (DE-600)1616-0 (DE-576)014400367 0010-7999 nnns volume:42 year:1973 number:4 month:12 pages:273-285 https://doi.org/10.1007/BF00372606 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_62 GBV_ILN_65 GBV_ILN_70 GBV_ILN_285 GBV_ILN_2001 GBV_ILN_2004 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4323 TE 1000 AR 42 1973 4 12 273-285 |
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10.1007/BF00372606 doi (DE-627)OLC2070485714 (DE-He213)BF00372606-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Menzies, Martin verfasserin aut Mineralogy and partial melt textures within an ultramafic-mafic body, Greece 1973 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1973 Abstract Ultramafic-mafic rocks from Makrirrakhi, Central Greece exhibit features of an original ophiolite sequence which contains depleted mantle material, ultramafic containing partial melt textures and possibly the mafic “pluton” which resulted from the coalescing of these partial melt segregations. Considerable mineralogical variation exists: unzoned olivine crystals range in composition from $ Fo_{78–84} $ (mafics) to $ Fo_{88–92} $ (ultramafics), plagioclases $ An_{64–79} $ (mafics) to $ An_{80–90} $ (ultramafics) and spinel varies from a chromian spinel (ultramafics) to a more aluminous-titaniferous spinel (mafics). Pyroxenes from the ultramafics display a limited range: $ En_{89–92} $ $ Fs_{9–8} $ $ Wo_{0–2} $ (orthopyroxene) and $ En_{48–54} $ $ Fs_{1–10} $ $ Wo_{38–50} $ (clinopyroxene). Mafic rocks display a greater range being richer in ferrosilite $ En_{36–65} $ $ Fs_{3–20} $ $ Wo_{33–51} $. Pyroxenes from within the partial melt segregations have chemical affinities with those from the gabbrotroctolite series. A model of partial melt within the upper mantle, and, a set of criteria to distinguish partial melt textures from cumulate textures, are developed from analytical data and textural evidence. Analytical Data Olivine Mineral Resource Limited Range Great Range Enthalten in Contributions to mineralogy and petrology Springer-Verlag, 1966 42(1973), 4 vom: Dez., Seite 273-285 (DE-627)129068721 (DE-600)1616-0 (DE-576)014400367 0010-7999 nnns volume:42 year:1973 number:4 month:12 pages:273-285 https://doi.org/10.1007/BF00372606 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_62 GBV_ILN_65 GBV_ILN_70 GBV_ILN_285 GBV_ILN_2001 GBV_ILN_2004 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4323 TE 1000 AR 42 1973 4 12 273-285 |
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10.1007/BF00372606 doi (DE-627)OLC2070485714 (DE-He213)BF00372606-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Menzies, Martin verfasserin aut Mineralogy and partial melt textures within an ultramafic-mafic body, Greece 1973 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1973 Abstract Ultramafic-mafic rocks from Makrirrakhi, Central Greece exhibit features of an original ophiolite sequence which contains depleted mantle material, ultramafic containing partial melt textures and possibly the mafic “pluton” which resulted from the coalescing of these partial melt segregations. Considerable mineralogical variation exists: unzoned olivine crystals range in composition from $ Fo_{78–84} $ (mafics) to $ Fo_{88–92} $ (ultramafics), plagioclases $ An_{64–79} $ (mafics) to $ An_{80–90} $ (ultramafics) and spinel varies from a chromian spinel (ultramafics) to a more aluminous-titaniferous spinel (mafics). Pyroxenes from the ultramafics display a limited range: $ En_{89–92} $ $ Fs_{9–8} $ $ Wo_{0–2} $ (orthopyroxene) and $ En_{48–54} $ $ Fs_{1–10} $ $ Wo_{38–50} $ (clinopyroxene). Mafic rocks display a greater range being richer in ferrosilite $ En_{36–65} $ $ Fs_{3–20} $ $ Wo_{33–51} $. Pyroxenes from within the partial melt segregations have chemical affinities with those from the gabbrotroctolite series. A model of partial melt within the upper mantle, and, a set of criteria to distinguish partial melt textures from cumulate textures, are developed from analytical data and textural evidence. Analytical Data Olivine Mineral Resource Limited Range Great Range Enthalten in Contributions to mineralogy and petrology Springer-Verlag, 1966 42(1973), 4 vom: Dez., Seite 273-285 (DE-627)129068721 (DE-600)1616-0 (DE-576)014400367 0010-7999 nnns volume:42 year:1973 number:4 month:12 pages:273-285 https://doi.org/10.1007/BF00372606 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_62 GBV_ILN_65 GBV_ILN_70 GBV_ILN_285 GBV_ILN_2001 GBV_ILN_2004 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4323 TE 1000 AR 42 1973 4 12 273-285 |
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10.1007/BF00372606 doi (DE-627)OLC2070485714 (DE-He213)BF00372606-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Menzies, Martin verfasserin aut Mineralogy and partial melt textures within an ultramafic-mafic body, Greece 1973 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1973 Abstract Ultramafic-mafic rocks from Makrirrakhi, Central Greece exhibit features of an original ophiolite sequence which contains depleted mantle material, ultramafic containing partial melt textures and possibly the mafic “pluton” which resulted from the coalescing of these partial melt segregations. Considerable mineralogical variation exists: unzoned olivine crystals range in composition from $ Fo_{78–84} $ (mafics) to $ Fo_{88–92} $ (ultramafics), plagioclases $ An_{64–79} $ (mafics) to $ An_{80–90} $ (ultramafics) and spinel varies from a chromian spinel (ultramafics) to a more aluminous-titaniferous spinel (mafics). Pyroxenes from the ultramafics display a limited range: $ En_{89–92} $ $ Fs_{9–8} $ $ Wo_{0–2} $ (orthopyroxene) and $ En_{48–54} $ $ Fs_{1–10} $ $ Wo_{38–50} $ (clinopyroxene). Mafic rocks display a greater range being richer in ferrosilite $ En_{36–65} $ $ Fs_{3–20} $ $ Wo_{33–51} $. Pyroxenes from within the partial melt segregations have chemical affinities with those from the gabbrotroctolite series. A model of partial melt within the upper mantle, and, a set of criteria to distinguish partial melt textures from cumulate textures, are developed from analytical data and textural evidence. Analytical Data Olivine Mineral Resource Limited Range Great Range Enthalten in Contributions to mineralogy and petrology Springer-Verlag, 1966 42(1973), 4 vom: Dez., Seite 273-285 (DE-627)129068721 (DE-600)1616-0 (DE-576)014400367 0010-7999 nnns volume:42 year:1973 number:4 month:12 pages:273-285 https://doi.org/10.1007/BF00372606 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_62 GBV_ILN_65 GBV_ILN_70 GBV_ILN_285 GBV_ILN_2001 GBV_ILN_2004 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4323 TE 1000 AR 42 1973 4 12 273-285 |
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10.1007/BF00372606 doi (DE-627)OLC2070485714 (DE-He213)BF00372606-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Menzies, Martin verfasserin aut Mineralogy and partial melt textures within an ultramafic-mafic body, Greece 1973 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1973 Abstract Ultramafic-mafic rocks from Makrirrakhi, Central Greece exhibit features of an original ophiolite sequence which contains depleted mantle material, ultramafic containing partial melt textures and possibly the mafic “pluton” which resulted from the coalescing of these partial melt segregations. Considerable mineralogical variation exists: unzoned olivine crystals range in composition from $ Fo_{78–84} $ (mafics) to $ Fo_{88–92} $ (ultramafics), plagioclases $ An_{64–79} $ (mafics) to $ An_{80–90} $ (ultramafics) and spinel varies from a chromian spinel (ultramafics) to a more aluminous-titaniferous spinel (mafics). Pyroxenes from the ultramafics display a limited range: $ En_{89–92} $ $ Fs_{9–8} $ $ Wo_{0–2} $ (orthopyroxene) and $ En_{48–54} $ $ Fs_{1–10} $ $ Wo_{38–50} $ (clinopyroxene). Mafic rocks display a greater range being richer in ferrosilite $ En_{36–65} $ $ Fs_{3–20} $ $ Wo_{33–51} $. Pyroxenes from within the partial melt segregations have chemical affinities with those from the gabbrotroctolite series. A model of partial melt within the upper mantle, and, a set of criteria to distinguish partial melt textures from cumulate textures, are developed from analytical data and textural evidence. Analytical Data Olivine Mineral Resource Limited Range Great Range Enthalten in Contributions to mineralogy and petrology Springer-Verlag, 1966 42(1973), 4 vom: Dez., Seite 273-285 (DE-627)129068721 (DE-600)1616-0 (DE-576)014400367 0010-7999 nnns volume:42 year:1973 number:4 month:12 pages:273-285 https://doi.org/10.1007/BF00372606 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_62 GBV_ILN_65 GBV_ILN_70 GBV_ILN_285 GBV_ILN_2001 GBV_ILN_2004 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4323 TE 1000 AR 42 1973 4 12 273-285 |
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Mineralogy and partial melt textures within an ultramafic-mafic body, Greece |
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Abstract Ultramafic-mafic rocks from Makrirrakhi, Central Greece exhibit features of an original ophiolite sequence which contains depleted mantle material, ultramafic containing partial melt textures and possibly the mafic “pluton” which resulted from the coalescing of these partial melt segregations. Considerable mineralogical variation exists: unzoned olivine crystals range in composition from $ Fo_{78–84} $ (mafics) to $ Fo_{88–92} $ (ultramafics), plagioclases $ An_{64–79} $ (mafics) to $ An_{80–90} $ (ultramafics) and spinel varies from a chromian spinel (ultramafics) to a more aluminous-titaniferous spinel (mafics). Pyroxenes from the ultramafics display a limited range: $ En_{89–92} $ $ Fs_{9–8} $ $ Wo_{0–2} $ (orthopyroxene) and $ En_{48–54} $ $ Fs_{1–10} $ $ Wo_{38–50} $ (clinopyroxene). Mafic rocks display a greater range being richer in ferrosilite $ En_{36–65} $ $ Fs_{3–20} $ $ Wo_{33–51} $. Pyroxenes from within the partial melt segregations have chemical affinities with those from the gabbrotroctolite series. A model of partial melt within the upper mantle, and, a set of criteria to distinguish partial melt textures from cumulate textures, are developed from analytical data and textural evidence. © Springer-Verlag 1973 |
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Abstract Ultramafic-mafic rocks from Makrirrakhi, Central Greece exhibit features of an original ophiolite sequence which contains depleted mantle material, ultramafic containing partial melt textures and possibly the mafic “pluton” which resulted from the coalescing of these partial melt segregations. Considerable mineralogical variation exists: unzoned olivine crystals range in composition from $ Fo_{78–84} $ (mafics) to $ Fo_{88–92} $ (ultramafics), plagioclases $ An_{64–79} $ (mafics) to $ An_{80–90} $ (ultramafics) and spinel varies from a chromian spinel (ultramafics) to a more aluminous-titaniferous spinel (mafics). Pyroxenes from the ultramafics display a limited range: $ En_{89–92} $ $ Fs_{9–8} $ $ Wo_{0–2} $ (orthopyroxene) and $ En_{48–54} $ $ Fs_{1–10} $ $ Wo_{38–50} $ (clinopyroxene). Mafic rocks display a greater range being richer in ferrosilite $ En_{36–65} $ $ Fs_{3–20} $ $ Wo_{33–51} $. Pyroxenes from within the partial melt segregations have chemical affinities with those from the gabbrotroctolite series. A model of partial melt within the upper mantle, and, a set of criteria to distinguish partial melt textures from cumulate textures, are developed from analytical data and textural evidence. © Springer-Verlag 1973 |
| abstract_unstemmed |
Abstract Ultramafic-mafic rocks from Makrirrakhi, Central Greece exhibit features of an original ophiolite sequence which contains depleted mantle material, ultramafic containing partial melt textures and possibly the mafic “pluton” which resulted from the coalescing of these partial melt segregations. Considerable mineralogical variation exists: unzoned olivine crystals range in composition from $ Fo_{78–84} $ (mafics) to $ Fo_{88–92} $ (ultramafics), plagioclases $ An_{64–79} $ (mafics) to $ An_{80–90} $ (ultramafics) and spinel varies from a chromian spinel (ultramafics) to a more aluminous-titaniferous spinel (mafics). Pyroxenes from the ultramafics display a limited range: $ En_{89–92} $ $ Fs_{9–8} $ $ Wo_{0–2} $ (orthopyroxene) and $ En_{48–54} $ $ Fs_{1–10} $ $ Wo_{38–50} $ (clinopyroxene). Mafic rocks display a greater range being richer in ferrosilite $ En_{36–65} $ $ Fs_{3–20} $ $ Wo_{33–51} $. Pyroxenes from within the partial melt segregations have chemical affinities with those from the gabbrotroctolite series. A model of partial melt within the upper mantle, and, a set of criteria to distinguish partial melt textures from cumulate textures, are developed from analytical data and textural evidence. © Springer-Verlag 1973 |
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