Resolving the Routine Presence of Kyanite, Andalusite and Sillimanite across a Region using Foliation Intersection/Inflection Axes Preserved in Porphyroblasts, Petrographic Observations and Thermobarometry-中国期刊网

摘要 ConstraintsfromP-Tpseudosections(MnNCKFMASHsystem),foliationintersection/inflectionaxespreservedinporphyroblasts(FIAs),mineralassemblagesandtexturalrelationshipsforrockscontainingallthreeAl2SiO5polymorphsindicateakyanite→andalusite→sillimanitesequentialformationatdifferenttimesratherthanstablecoexistenceattheAl2SiO5triplepoint.AllthreeAl2SiO5polymorphsgrewintheChl,Bt,Ms,Grt,St,PlandCrdbearingOrdovicianClayholeSchistinBalcooma,northeasternAustraliaseparatelyalongaloopedP-T-t-Dpaththatswapsfromclockwisetoanticlockwiseinthetectono-metamorphichistoryoftheregion.KyanitegrewduringcrustalthickeninginanEarlySilurianOrogeniceventfollowedbydecompression/heating,andalusiteandfibroliticsillimanitegrowthduringEarlyDevonianexhumation.

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Resolving the Routine Presence of Kyanite, Andalusite and Sillimanite across a Region using Foliation Intersection/Inflection Axes Preserved in Porphyroblasts, Petrographic Observations and Thermobarometry

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Resolving the Routine Presence of Kyanite, Andalusite and Sillimanite across a Region using Foliation Intersection/Inflection Axes Preserved in Porphyroblasts, Petrographic Observations and Thermobarometry

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