The Contribution of Volume Change in Preserving High‐P Metastable Assemblages.

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Title: The Contribution of Volume Change in Preserving High‐P Metastable Assemblages.
Authors: Chapman, Timothy1 (AUTHOR) timothy.chapman@une.edu.au, Clarke, Geoffrey L.2 (AUTHOR), Piazolo, Sandra3 (AUTHOR)
Source: Journal of Metamorphic Geology. Apr2026, Vol. 44 Issue 3, p177-199. 23p.
Subject Terms: *Pyroxene, *Albite, *Metamorphism (Geology), *Minerals, *Recrystallization (Metallurgy), *Tectonic exhumation
Geographic Terms: New Caledonia
Abstract: Incomplete retrograde reaction of sodic–calcic pyroxene occurred during the exhumation of Eocene eclogite and blueschist in NE New Caledonia. Sodic–calcic pyroxene is well‐preserved in reaction relationships with paragonite and structurally late albite, in conflict with the prediction that it should transform efficiently during decompression to albite, paragonite, glaucophane and quartz. The microstructural distribution of albite accompanying crenulation cleavage development is consistent with albite growth having been restricted by space‐filling requirements. In contrast, domains of high strain enable the accommodation of volume and fluid infiltration, increasing the size of the equilibration volume leading to the complete conversion of sodic–calcic clinopyroxene to albite. Despite decompression‐driven dehydration, limited volume accommodation presents a plausible mechanism to metastably preserve high‐P (up to 18 kbar) sodic–calcic clinopyroxene‐bearing assemblages to lower‐P conditions (~10 kbar) that should stabilise albite. Efficient retrogression is facilitated by dynamic recrystallisation inducing dilation. [ABSTRACT FROM AUTHOR]
Database: Energy & Power Source
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Header DbId: enr
DbLabel: Energy & Power Source
An: 192092287
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PubType: Academic Journal
PubTypeId: academicJournal
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  Data: The Contribution of Volume Change in Preserving High‐P Metastable Assemblages.
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  Data: <searchLink fieldCode="AR" term="%22Chapman%2C+Timothy%22">Chapman, Timothy</searchLink><relatesTo>1</relatesTo> (AUTHOR)<i> timothy.chapman@une.edu.au</i><br /><searchLink fieldCode="AR" term="%22Clarke%2C+Geoffrey L%2E%22">Clarke, Geoffrey L.</searchLink><relatesTo>2</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Piazolo%2C+Sandra%22">Piazolo, Sandra</searchLink><relatesTo>3</relatesTo> (AUTHOR)
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  Data: <searchLink fieldCode="JN" term="%22Journal+of+Metamorphic+Geology%22">Journal of Metamorphic Geology</searchLink>. Apr2026, Vol. 44 Issue 3, p177-199. 23p.
– Name: Subject
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  Data: *<searchLink fieldCode="DE" term="%22Pyroxene%22">Pyroxene</searchLink><br />*<searchLink fieldCode="DE" term="%22Albite%22">Albite</searchLink><br />*<searchLink fieldCode="DE" term="%22Metamorphism+%28Geology%29%22">Metamorphism (Geology)</searchLink><br />*<searchLink fieldCode="DE" term="%22Minerals%22">Minerals</searchLink><br />*<searchLink fieldCode="DE" term="%22Recrystallization+%28Metallurgy%29%22">Recrystallization (Metallurgy)</searchLink><br />*<searchLink fieldCode="DE" term="%22Tectonic+exhumation%22">Tectonic exhumation</searchLink>
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  Data: <searchLink fieldCode="DE" term="%22New+Caledonia%22">New Caledonia</searchLink>
– Name: Abstract
  Label: Abstract
  Group: Ab
  Data: Incomplete retrograde reaction of sodic–calcic pyroxene occurred during the exhumation of Eocene eclogite and blueschist in NE New Caledonia. Sodic–calcic pyroxene is well‐preserved in reaction relationships with paragonite and structurally late albite, in conflict with the prediction that it should transform efficiently during decompression to albite, paragonite, glaucophane and quartz. The microstructural distribution of albite accompanying crenulation cleavage development is consistent with albite growth having been restricted by space‐filling requirements. In contrast, domains of high strain enable the accommodation of volume and fluid infiltration, increasing the size of the equilibration volume leading to the complete conversion of sodic–calcic clinopyroxene to albite. Despite decompression‐driven dehydration, limited volume accommodation presents a plausible mechanism to metastably preserve high‐P (up to 18 kbar) sodic–calcic clinopyroxene‐bearing assemblages to lower‐P conditions (~10 kbar) that should stabilise albite. Efficient retrogression is facilitated by dynamic recrystallisation inducing dilation. [ABSTRACT FROM AUTHOR]
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RecordInfo BibRecord:
  BibEntity:
    Identifiers:
      – Type: doi
        Value: 10.1111/jmg.70028
    Languages:
      – Code: eng
        Text: English
    PhysicalDescription:
      Pagination:
        PageCount: 23
        StartPage: 177
    Subjects:
      – SubjectFull: Pyroxene
        Type: general
      – SubjectFull: Albite
        Type: general
      – SubjectFull: Metamorphism (Geology)
        Type: general
      – SubjectFull: Minerals
        Type: general
      – SubjectFull: Recrystallization (Metallurgy)
        Type: general
      – SubjectFull: Tectonic exhumation
        Type: general
      – SubjectFull: New Caledonia
        Type: general
    Titles:
      – TitleFull: The Contribution of Volume Change in Preserving High‐P Metastable Assemblages.
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          Name:
            NameFull: Chapman, Timothy
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          Name:
            NameFull: Clarke, Geoffrey L.
      – PersonEntity:
          Name:
            NameFull: Piazolo, Sandra
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          Dates:
            – D: 01
              M: 04
              Text: Apr2026
              Type: published
              Y: 2026
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              Value: 44
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          Titles:
            – TitleFull: Journal of Metamorphic Geology
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