Retrograde mineral and fluid evolution in high-pressure metapelites (Schistes Lustres unit, Western Alps).

Ph. Agard; B. Goffe; J.L.R. Touret; O. Vidal

doi:10.1007/s004100000190

Retrograde mineral and fluid evolution in high-pressure metapelites (Schistes Lustres unit, Western Alps).

Ph. Agard, B. Goffe, J.L.R. Touret, O. Vidal

Research output: Contribution to Journal › Article › Academic › peer-review

Abstract

Fluid inclusions have been analysed in successive generations of syn-metamorphic segregations within low-grade, high-pressure, low-temperature (HP-LT) metapelites from the Western Alps. Fluid composition was then compared to mass transfer deduced from outcrop-scale retrograde mineral reactions. Two types of quartz segregations (veins) occur in the 'Schistes lustres' unit: early blueschist-facies carpholite-bearing veins (BS) and retrograde greenschist-facies chlorite-bearing veins (GS). Fluid inclusions in both types of segregations are aqueous (no trace of dissolved gases such as CO

Original language	English
Pages (from-to)	296-315
Journal	Contributions to Mineralogy and Petrology
Volume	140
DOIs	https://doi.org/10.1007/s004100000190
Publication status	Published - 2000

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title = "Retrograde mineral and fluid evolution in high-pressure metapelites (Schistes Lustres unit, Western Alps).",

abstract = "Fluid inclusions have been analysed in successive generations of syn-metamorphic segregations within low-grade, high-pressure, low-temperature (HP-LT) metapelites from the Western Alps. Fluid composition was then compared to mass transfer deduced from outcrop-scale retrograde mineral reactions. Two types of quartz segregations (veins) occur in the 'Schistes lustres' unit: early blueschist-facies carpholite-bearing veins (BS) and retrograde greenschist-facies chlorite-bearing veins (GS). Fluid inclusions in both types of segregations are aqueous (no trace of dissolved gases such as CO",

author = "Ph. Agard and B. Goffe and J.L.R. Touret and O. Vidal",

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doi = "10.1007/s004100000190",

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AU - Agard, Ph.

AU - Goffe, B.

AU - Touret, J.L.R.

AU - Vidal, O.

PY - 2000

Y1 - 2000

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AB - Fluid inclusions have been analysed in successive generations of syn-metamorphic segregations within low-grade, high-pressure, low-temperature (HP-LT) metapelites from the Western Alps. Fluid composition was then compared to mass transfer deduced from outcrop-scale retrograde mineral reactions. Two types of quartz segregations (veins) occur in the 'Schistes lustres' unit: early blueschist-facies carpholite-bearing veins (BS) and retrograde greenschist-facies chlorite-bearing veins (GS). Fluid inclusions in both types of segregations are aqueous (no trace of dissolved gases such as CO

U2 - 10.1007/s004100000190

DO - 10.1007/s004100000190

M3 - Article

VL - 140

SP - 296

EP - 315

JO - Contributions to Mineralogy and Petrology

JF - Contributions to Mineralogy and Petrology

SN - 0010-7999

ER -

Retrograde mineral and fluid evolution in high-pressure metapelites (Schistes Lustres unit, Western Alps).

Abstract

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