Distinguishing melting of heterogeneous mantle sources from crustal contamination: Insights from Sr isotopes at the Phenocryst Scale, Pisgah Crater, California

F. C. Ramos, Mary Reid

Research output: Contribution to journalArticle

27 Citations (Scopus)

Abstract

Compositionally heterogeneous basaltic centers from a variety of tectonic environments, including Pisgah Crater in the Mojave Desert region of California, exhibit secular changes in their chemistry that might be explained by the sequential melting of ultramafic to mafic mantle sources. We have analyzed phenocrysts from alkali basalts and hawaiites erupted at Pisgah Crater to investiqate the effects of open-system modifications imposed on basaltic systems. We present 87Sr/ 86Sr data for individual phenocrysts of amphibole and clinopyroxene and the first published results of single olivine grains, in addition to plagioclase. Each mineral phase exhibits a range in Sr isotope composition that may only partially overlap the isotopic composition of the other mineral phases, suggesting an interplay between two magmatic end-members that continued up to the time of eruption. Limited 87Sr/ 86Sr variability in minerals from early and intermediate lavas indicates only moderate syn-crystallization open-system modification, whereas minerals in late-erupted lavas have much higher 87Sr/86Sr, consistent with extensive open-system modification. Rimward increases in 87Sr/86Sr of plagioclase confirm that these changes occurred within the stability field of plagioclase and, therefore, at crustal or near-crustal depths. The major element compositions of olivine-hosted melt inclusions indicate that an Al-rich component of andesitic composition (87Sr/86Sr ≥0·7056), possibly derived from plagioclase-rich cumulates or pelites, was assimilated by magma generated from asthenosphere or young lithosphere with 87Sr/86Sr ≤0·7038. The results clearly demonstrate the utility of measuring the 87Sr/86Sr of individual minerals and indicate that Pisgah Crater basalts probably acquired isotopically enriched geochemical signatures from crustal contamination, rather than from mixing of heterogeneous mantle melts.

Original languageEnglish (US)
Pages (from-to)999-1012
Number of pages14
JournalJournal of Petrology
Volume46
Issue number5
DOIs
StatePublished - May 2005

Fingerprint

phenocryst
crustal contamination
craters
mantle source
Isotopes
crater
Minerals
plagioclase
Earth mantle
contamination
Melting
Contamination
isotopes
melting
minerals
isotope
Open systems
mineral
Chemical analysis
olivine

Keywords

  • Assimilation
  • Basalts
  • Melt inclusions
  • Minerals
  • Sr isotopes

ASJC Scopus subject areas

  • Geochemistry and Petrology
  • Geophysics

Cite this

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title = "Distinguishing melting of heterogeneous mantle sources from crustal contamination: Insights from Sr isotopes at the Phenocryst Scale, Pisgah Crater, California",
abstract = "Compositionally heterogeneous basaltic centers from a variety of tectonic environments, including Pisgah Crater in the Mojave Desert region of California, exhibit secular changes in their chemistry that might be explained by the sequential melting of ultramafic to mafic mantle sources. We have analyzed phenocrysts from alkali basalts and hawaiites erupted at Pisgah Crater to investiqate the effects of open-system modifications imposed on basaltic systems. We present 87Sr/ 86Sr data for individual phenocrysts of amphibole and clinopyroxene and the first published results of single olivine grains, in addition to plagioclase. Each mineral phase exhibits a range in Sr isotope composition that may only partially overlap the isotopic composition of the other mineral phases, suggesting an interplay between two magmatic end-members that continued up to the time of eruption. Limited 87Sr/ 86Sr variability in minerals from early and intermediate lavas indicates only moderate syn-crystallization open-system modification, whereas minerals in late-erupted lavas have much higher 87Sr/86Sr, consistent with extensive open-system modification. Rimward increases in 87Sr/86Sr of plagioclase confirm that these changes occurred within the stability field of plagioclase and, therefore, at crustal or near-crustal depths. The major element compositions of olivine-hosted melt inclusions indicate that an Al-rich component of andesitic composition (87Sr/86Sr ≥0·7056), possibly derived from plagioclase-rich cumulates or pelites, was assimilated by magma generated from asthenosphere or young lithosphere with 87Sr/86Sr ≤0·7038. The results clearly demonstrate the utility of measuring the 87Sr/86Sr of individual minerals and indicate that Pisgah Crater basalts probably acquired isotopically enriched geochemical signatures from crustal contamination, rather than from mixing of heterogeneous mantle melts.",
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N2 - Compositionally heterogeneous basaltic centers from a variety of tectonic environments, including Pisgah Crater in the Mojave Desert region of California, exhibit secular changes in their chemistry that might be explained by the sequential melting of ultramafic to mafic mantle sources. We have analyzed phenocrysts from alkali basalts and hawaiites erupted at Pisgah Crater to investiqate the effects of open-system modifications imposed on basaltic systems. We present 87Sr/ 86Sr data for individual phenocrysts of amphibole and clinopyroxene and the first published results of single olivine grains, in addition to plagioclase. Each mineral phase exhibits a range in Sr isotope composition that may only partially overlap the isotopic composition of the other mineral phases, suggesting an interplay between two magmatic end-members that continued up to the time of eruption. Limited 87Sr/ 86Sr variability in minerals from early and intermediate lavas indicates only moderate syn-crystallization open-system modification, whereas minerals in late-erupted lavas have much higher 87Sr/86Sr, consistent with extensive open-system modification. Rimward increases in 87Sr/86Sr of plagioclase confirm that these changes occurred within the stability field of plagioclase and, therefore, at crustal or near-crustal depths. The major element compositions of olivine-hosted melt inclusions indicate that an Al-rich component of andesitic composition (87Sr/86Sr ≥0·7056), possibly derived from plagioclase-rich cumulates or pelites, was assimilated by magma generated from asthenosphere or young lithosphere with 87Sr/86Sr ≤0·7038. The results clearly demonstrate the utility of measuring the 87Sr/86Sr of individual minerals and indicate that Pisgah Crater basalts probably acquired isotopically enriched geochemical signatures from crustal contamination, rather than from mixing of heterogeneous mantle melts.

AB - Compositionally heterogeneous basaltic centers from a variety of tectonic environments, including Pisgah Crater in the Mojave Desert region of California, exhibit secular changes in their chemistry that might be explained by the sequential melting of ultramafic to mafic mantle sources. We have analyzed phenocrysts from alkali basalts and hawaiites erupted at Pisgah Crater to investiqate the effects of open-system modifications imposed on basaltic systems. We present 87Sr/ 86Sr data for individual phenocrysts of amphibole and clinopyroxene and the first published results of single olivine grains, in addition to plagioclase. Each mineral phase exhibits a range in Sr isotope composition that may only partially overlap the isotopic composition of the other mineral phases, suggesting an interplay between two magmatic end-members that continued up to the time of eruption. Limited 87Sr/ 86Sr variability in minerals from early and intermediate lavas indicates only moderate syn-crystallization open-system modification, whereas minerals in late-erupted lavas have much higher 87Sr/86Sr, consistent with extensive open-system modification. Rimward increases in 87Sr/86Sr of plagioclase confirm that these changes occurred within the stability field of plagioclase and, therefore, at crustal or near-crustal depths. The major element compositions of olivine-hosted melt inclusions indicate that an Al-rich component of andesitic composition (87Sr/86Sr ≥0·7056), possibly derived from plagioclase-rich cumulates or pelites, was assimilated by magma generated from asthenosphere or young lithosphere with 87Sr/86Sr ≤0·7038. The results clearly demonstrate the utility of measuring the 87Sr/86Sr of individual minerals and indicate that Pisgah Crater basalts probably acquired isotopically enriched geochemical signatures from crustal contamination, rather than from mixing of heterogeneous mantle melts.

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