Oxygen and hydrogen isotope compositions of eclogites and associated rocks from the Eastern Sesia zone (Western Alps, Italy)

Abstract Oxygen and hydrogen isotope analyses have been made of mineral separates from eclogites, glaucophanites and glaucophane schists from the eastern Sesia zone (Italian Western Alps). Regularities in (1) hydrogen isotope compositions, (2) order of 18O enrichment among coexisting minerals, and (...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Desmons, Jacqueline [verfasserIn] O'Neil, James R.

Format:	Artikel
Sprache:	Englisch

Erschienen:	1978

Schlagwörter:	Rutile Subduction Isotope Analysis Oxygen Isotope Isotope Fractionation

Systematik:	TE 1000

Anmerkung:	© Springer-Verlag 1978

Übergeordnetes Werk:	Enthalten in: Contributions to mineralogy and petrology - Springer-Verlag, 1966, 67(1978), 1 vom: Aug., Seite 79-85
Übergeordnetes Werk:	volume:67 ; year:1978 ; number:1 ; month:08 ; pages:79-85

Links:	Volltext

DOI / URN:	10.1007/BF00371635

Katalog-ID:	OLC207049179X

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520			\|a Abstract Oxygen and hydrogen isotope analyses have been made of mineral separates from eclogites, glaucophanites and glaucophane schists from the eastern Sesia zone (Italian Western Alps). Regularities in (1) hydrogen isotope compositions, (2) order of 18O enrichment among coexisting minerals, and (3) Δ 18O (quartz-rutile) and Δ 18O (quartz-phengite) imply attainment of a high degree of isotopic equilibrium. However, some scattering of $ δ^{18} $O values of individual minerals indicates that the eclogitic assemblage did not form in the presence of a thoroughly pervasive fluid. Minerals from an eclogitic lens enclosed in marble have $ δ^{18} $O values distinctly different from those measured in the other rocks. The $ δ^{18} $O values are high in comparison with other type C eclogites of the world, and it is proposed that the fluid present during the high pressure metamorphism has to a large extent been inherited from the precursor rocks of amphibolite facies. An average formation temperature of 540 ° C is inferred from the oxygen isotope fractionations between quartz and rutile and between quartz and white mica. This temperature is in accordance with petrologic considerations and implies subduction of the precursor rocks into the upper mantle to achieve the high pressures required.
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allfields	10.1007/BF00371635 doi (DE-627)OLC207049179X (DE-He213)BF00371635-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Desmons, Jacqueline verfasserin aut Oxygen and hydrogen isotope compositions of eclogites and associated rocks from the Eastern Sesia zone (Western Alps, Italy) 1978 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1978 Abstract Oxygen and hydrogen isotope analyses have been made of mineral separates from eclogites, glaucophanites and glaucophane schists from the eastern Sesia zone (Italian Western Alps). Regularities in (1) hydrogen isotope compositions, (2) order of 18O enrichment among coexisting minerals, and (3) Δ 18O (quartz-rutile) and Δ 18O (quartz-phengite) imply attainment of a high degree of isotopic equilibrium. However, some scattering of $ δ^{18} $O values of individual minerals indicates that the eclogitic assemblage did not form in the presence of a thoroughly pervasive fluid. Minerals from an eclogitic lens enclosed in marble have $ δ^{18} $O values distinctly different from those measured in the other rocks. The $ δ^{18} $O values are high in comparison with other type C eclogites of the world, and it is proposed that the fluid present during the high pressure metamorphism has to a large extent been inherited from the precursor rocks of amphibolite facies. An average formation temperature of 540 ° C is inferred from the oxygen isotope fractionations between quartz and rutile and between quartz and white mica. This temperature is in accordance with petrologic considerations and implies subduction of the precursor rocks into the upper mantle to achieve the high pressures required. Rutile Subduction Isotope Analysis Oxygen Isotope Isotope Fractionation O'Neil, James R. aut Enthalten in Contributions to mineralogy and petrology Springer-Verlag, 1966 67(1978), 1 vom: Aug., Seite 79-85 (DE-627)129068721 (DE-600)1616-0 (DE-576)014400367 0010-7999 nnns volume:67 year:1978 number:1 month:08 pages:79-85 https://doi.org/10.1007/BF00371635 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_40 GBV_ILN_62 GBV_ILN_65 GBV_ILN_70 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_4305 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4323 TE 1000 AR 67 1978 1 08 79-85
spelling	10.1007/BF00371635 doi (DE-627)OLC207049179X (DE-He213)BF00371635-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Desmons, Jacqueline verfasserin aut Oxygen and hydrogen isotope compositions of eclogites and associated rocks from the Eastern Sesia zone (Western Alps, Italy) 1978 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1978 Abstract Oxygen and hydrogen isotope analyses have been made of mineral separates from eclogites, glaucophanites and glaucophane schists from the eastern Sesia zone (Italian Western Alps). Regularities in (1) hydrogen isotope compositions, (2) order of 18O enrichment among coexisting minerals, and (3) Δ 18O (quartz-rutile) and Δ 18O (quartz-phengite) imply attainment of a high degree of isotopic equilibrium. However, some scattering of $ δ^{18} $O values of individual minerals indicates that the eclogitic assemblage did not form in the presence of a thoroughly pervasive fluid. Minerals from an eclogitic lens enclosed in marble have $ δ^{18} $O values distinctly different from those measured in the other rocks. The $ δ^{18} $O values are high in comparison with other type C eclogites of the world, and it is proposed that the fluid present during the high pressure metamorphism has to a large extent been inherited from the precursor rocks of amphibolite facies. An average formation temperature of 540 ° C is inferred from the oxygen isotope fractionations between quartz and rutile and between quartz and white mica. This temperature is in accordance with petrologic considerations and implies subduction of the precursor rocks into the upper mantle to achieve the high pressures required. Rutile Subduction Isotope Analysis Oxygen Isotope Isotope Fractionation O'Neil, James R. aut Enthalten in Contributions to mineralogy and petrology Springer-Verlag, 1966 67(1978), 1 vom: Aug., Seite 79-85 (DE-627)129068721 (DE-600)1616-0 (DE-576)014400367 0010-7999 nnns volume:67 year:1978 number:1 month:08 pages:79-85 https://doi.org/10.1007/BF00371635 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_40 GBV_ILN_62 GBV_ILN_65 GBV_ILN_70 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_4305 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4323 TE 1000 AR 67 1978 1 08 79-85
allfields_unstemmed	10.1007/BF00371635 doi (DE-627)OLC207049179X (DE-He213)BF00371635-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Desmons, Jacqueline verfasserin aut Oxygen and hydrogen isotope compositions of eclogites and associated rocks from the Eastern Sesia zone (Western Alps, Italy) 1978 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1978 Abstract Oxygen and hydrogen isotope analyses have been made of mineral separates from eclogites, glaucophanites and glaucophane schists from the eastern Sesia zone (Italian Western Alps). Regularities in (1) hydrogen isotope compositions, (2) order of 18O enrichment among coexisting minerals, and (3) Δ 18O (quartz-rutile) and Δ 18O (quartz-phengite) imply attainment of a high degree of isotopic equilibrium. However, some scattering of $ δ^{18} $O values of individual minerals indicates that the eclogitic assemblage did not form in the presence of a thoroughly pervasive fluid. Minerals from an eclogitic lens enclosed in marble have $ δ^{18} $O values distinctly different from those measured in the other rocks. The $ δ^{18} $O values are high in comparison with other type C eclogites of the world, and it is proposed that the fluid present during the high pressure metamorphism has to a large extent been inherited from the precursor rocks of amphibolite facies. An average formation temperature of 540 ° C is inferred from the oxygen isotope fractionations between quartz and rutile and between quartz and white mica. This temperature is in accordance with petrologic considerations and implies subduction of the precursor rocks into the upper mantle to achieve the high pressures required. Rutile Subduction Isotope Analysis Oxygen Isotope Isotope Fractionation O'Neil, James R. aut Enthalten in Contributions to mineralogy and petrology Springer-Verlag, 1966 67(1978), 1 vom: Aug., Seite 79-85 (DE-627)129068721 (DE-600)1616-0 (DE-576)014400367 0010-7999 nnns volume:67 year:1978 number:1 month:08 pages:79-85 https://doi.org/10.1007/BF00371635 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_40 GBV_ILN_62 GBV_ILN_65 GBV_ILN_70 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_4305 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4323 TE 1000 AR 67 1978 1 08 79-85
allfieldsGer	10.1007/BF00371635 doi (DE-627)OLC207049179X (DE-He213)BF00371635-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Desmons, Jacqueline verfasserin aut Oxygen and hydrogen isotope compositions of eclogites and associated rocks from the Eastern Sesia zone (Western Alps, Italy) 1978 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1978 Abstract Oxygen and hydrogen isotope analyses have been made of mineral separates from eclogites, glaucophanites and glaucophane schists from the eastern Sesia zone (Italian Western Alps). Regularities in (1) hydrogen isotope compositions, (2) order of 18O enrichment among coexisting minerals, and (3) Δ 18O (quartz-rutile) and Δ 18O (quartz-phengite) imply attainment of a high degree of isotopic equilibrium. However, some scattering of $ δ^{18} $O values of individual minerals indicates that the eclogitic assemblage did not form in the presence of a thoroughly pervasive fluid. Minerals from an eclogitic lens enclosed in marble have $ δ^{18} $O values distinctly different from those measured in the other rocks. The $ δ^{18} $O values are high in comparison with other type C eclogites of the world, and it is proposed that the fluid present during the high pressure metamorphism has to a large extent been inherited from the precursor rocks of amphibolite facies. An average formation temperature of 540 ° C is inferred from the oxygen isotope fractionations between quartz and rutile and between quartz and white mica. This temperature is in accordance with petrologic considerations and implies subduction of the precursor rocks into the upper mantle to achieve the high pressures required. Rutile Subduction Isotope Analysis Oxygen Isotope Isotope Fractionation O'Neil, James R. aut Enthalten in Contributions to mineralogy and petrology Springer-Verlag, 1966 67(1978), 1 vom: Aug., Seite 79-85 (DE-627)129068721 (DE-600)1616-0 (DE-576)014400367 0010-7999 nnns volume:67 year:1978 number:1 month:08 pages:79-85 https://doi.org/10.1007/BF00371635 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_40 GBV_ILN_62 GBV_ILN_65 GBV_ILN_70 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_4305 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4323 TE 1000 AR 67 1978 1 08 79-85
allfieldsSound	10.1007/BF00371635 doi (DE-627)OLC207049179X (DE-He213)BF00371635-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Desmons, Jacqueline verfasserin aut Oxygen and hydrogen isotope compositions of eclogites and associated rocks from the Eastern Sesia zone (Western Alps, Italy) 1978 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1978 Abstract Oxygen and hydrogen isotope analyses have been made of mineral separates from eclogites, glaucophanites and glaucophane schists from the eastern Sesia zone (Italian Western Alps). Regularities in (1) hydrogen isotope compositions, (2) order of 18O enrichment among coexisting minerals, and (3) Δ 18O (quartz-rutile) and Δ 18O (quartz-phengite) imply attainment of a high degree of isotopic equilibrium. However, some scattering of $ δ^{18} $O values of individual minerals indicates that the eclogitic assemblage did not form in the presence of a thoroughly pervasive fluid. Minerals from an eclogitic lens enclosed in marble have $ δ^{18} $O values distinctly different from those measured in the other rocks. The $ δ^{18} $O values are high in comparison with other type C eclogites of the world, and it is proposed that the fluid present during the high pressure metamorphism has to a large extent been inherited from the precursor rocks of amphibolite facies. An average formation temperature of 540 ° C is inferred from the oxygen isotope fractionations between quartz and rutile and between quartz and white mica. This temperature is in accordance with petrologic considerations and implies subduction of the precursor rocks into the upper mantle to achieve the high pressures required. Rutile Subduction Isotope Analysis Oxygen Isotope Isotope Fractionation O'Neil, James R. aut Enthalten in Contributions to mineralogy and petrology Springer-Verlag, 1966 67(1978), 1 vom: Aug., Seite 79-85 (DE-627)129068721 (DE-600)1616-0 (DE-576)014400367 0010-7999 nnns volume:67 year:1978 number:1 month:08 pages:79-85 https://doi.org/10.1007/BF00371635 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_40 GBV_ILN_62 GBV_ILN_65 GBV_ILN_70 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_4305 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4323 TE 1000 AR 67 1978 1 08 79-85
language	English
source	Enthalten in Contributions to mineralogy and petrology 67(1978), 1 vom: Aug., Seite 79-85 volume:67 year:1978 number:1 month:08 pages:79-85
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topic_facet	Rutile Subduction Isotope Analysis Oxygen Isotope Isotope Fractionation
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container_title	Contributions to mineralogy and petrology
authorswithroles_txt_mv	Desmons, Jacqueline @@aut@@ O'Neil, James R. @@aut@@
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author	Desmons, Jacqueline
spellingShingle	Desmons, Jacqueline ddc 550 ssgn 13 rvk TE 1000 misc Rutile misc Subduction misc Isotope Analysis misc Oxygen Isotope misc Isotope Fractionation Oxygen and hydrogen isotope compositions of eclogites and associated rocks from the Eastern Sesia zone (Western Alps, Italy)
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topic_title	550 VZ 13 ssgn TE 1000 VZ rvk Oxygen and hydrogen isotope compositions of eclogites and associated rocks from the Eastern Sesia zone (Western Alps, Italy) Rutile Subduction Isotope Analysis Oxygen Isotope Isotope Fractionation
topic	ddc 550 ssgn 13 rvk TE 1000 misc Rutile misc Subduction misc Isotope Analysis misc Oxygen Isotope misc Isotope Fractionation
topic_unstemmed	ddc 550 ssgn 13 rvk TE 1000 misc Rutile misc Subduction misc Isotope Analysis misc Oxygen Isotope misc Isotope Fractionation
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title	Oxygen and hydrogen isotope compositions of eclogites and associated rocks from the Eastern Sesia zone (Western Alps, Italy)
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title_full	Oxygen and hydrogen isotope compositions of eclogites and associated rocks from the Eastern Sesia zone (Western Alps, Italy)
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author_browse	Desmons, Jacqueline O'Neil, James R.
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title_sort	oxygen and hydrogen isotope compositions of eclogites and associated rocks from the eastern sesia zone (western alps, italy)
title_auth	Oxygen and hydrogen isotope compositions of eclogites and associated rocks from the Eastern Sesia zone (Western Alps, Italy)
abstract	Abstract Oxygen and hydrogen isotope analyses have been made of mineral separates from eclogites, glaucophanites and glaucophane schists from the eastern Sesia zone (Italian Western Alps). Regularities in (1) hydrogen isotope compositions, (2) order of 18O enrichment among coexisting minerals, and (3) Δ 18O (quartz-rutile) and Δ 18O (quartz-phengite) imply attainment of a high degree of isotopic equilibrium. However, some scattering of $ δ^{18} $O values of individual minerals indicates that the eclogitic assemblage did not form in the presence of a thoroughly pervasive fluid. Minerals from an eclogitic lens enclosed in marble have $ δ^{18} $O values distinctly different from those measured in the other rocks. The $ δ^{18} $O values are high in comparison with other type C eclogites of the world, and it is proposed that the fluid present during the high pressure metamorphism has to a large extent been inherited from the precursor rocks of amphibolite facies. An average formation temperature of 540 ° C is inferred from the oxygen isotope fractionations between quartz and rutile and between quartz and white mica. This temperature is in accordance with petrologic considerations and implies subduction of the precursor rocks into the upper mantle to achieve the high pressures required. © Springer-Verlag 1978
abstractGer	Abstract Oxygen and hydrogen isotope analyses have been made of mineral separates from eclogites, glaucophanites and glaucophane schists from the eastern Sesia zone (Italian Western Alps). Regularities in (1) hydrogen isotope compositions, (2) order of 18O enrichment among coexisting minerals, and (3) Δ 18O (quartz-rutile) and Δ 18O (quartz-phengite) imply attainment of a high degree of isotopic equilibrium. However, some scattering of $ δ^{18} $O values of individual minerals indicates that the eclogitic assemblage did not form in the presence of a thoroughly pervasive fluid. Minerals from an eclogitic lens enclosed in marble have $ δ^{18} $O values distinctly different from those measured in the other rocks. The $ δ^{18} $O values are high in comparison with other type C eclogites of the world, and it is proposed that the fluid present during the high pressure metamorphism has to a large extent been inherited from the precursor rocks of amphibolite facies. An average formation temperature of 540 ° C is inferred from the oxygen isotope fractionations between quartz and rutile and between quartz and white mica. This temperature is in accordance with petrologic considerations and implies subduction of the precursor rocks into the upper mantle to achieve the high pressures required. © Springer-Verlag 1978
abstract_unstemmed	Abstract Oxygen and hydrogen isotope analyses have been made of mineral separates from eclogites, glaucophanites and glaucophane schists from the eastern Sesia zone (Italian Western Alps). Regularities in (1) hydrogen isotope compositions, (2) order of 18O enrichment among coexisting minerals, and (3) Δ 18O (quartz-rutile) and Δ 18O (quartz-phengite) imply attainment of a high degree of isotopic equilibrium. However, some scattering of $ δ^{18} $O values of individual minerals indicates that the eclogitic assemblage did not form in the presence of a thoroughly pervasive fluid. Minerals from an eclogitic lens enclosed in marble have $ δ^{18} $O values distinctly different from those measured in the other rocks. The $ δ^{18} $O values are high in comparison with other type C eclogites of the world, and it is proposed that the fluid present during the high pressure metamorphism has to a large extent been inherited from the precursor rocks of amphibolite facies. An average formation temperature of 540 ° C is inferred from the oxygen isotope fractionations between quartz and rutile and between quartz and white mica. This temperature is in accordance with petrologic considerations and implies subduction of the precursor rocks into the upper mantle to achieve the high pressures required. © Springer-Verlag 1978
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title_short	Oxygen and hydrogen isotope compositions of eclogites and associated rocks from the Eastern Sesia zone (Western Alps, Italy)
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