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Titolo:
Recalibration of the GASP geobarometer in light of recent garnet and plagioclase activity models and versions of the garnet-biotite geothermometer
Autore:
Holdaway, MJ;
Indirizzi:
So Methodist Univ, Dept Geol Sci, Dallas, TX 75275 USA So Methodist Univ Dallas TX USA 75275 Dept Geol Sci, Dallas, TX 75275 USA
Titolo Testata:
AMERICAN MINERALOGIST
fascicolo: 10, volume: 86, anno: 2001,
pagine: 1117 - 1129
SICI:
0003-004X(200110)86:10<1117:ROTGGI>2.0.ZU;2-8
Fonte:
ISI
Lingua:
ENG
Soggetto:
SOUTH-CENTRAL MAINE; WEST-CENTRAL MAINE; MIXING PROPERTIES; BRITISH-COLUMBIA; METAMORPHIC REACTIONS; THERMODYNAMIC MODELS; PELITIC SCHISTS; NORTHERN IDAHO; NEW-HAMPSHIRE; SNOW PEAK;
Tipo documento:
Article
Natura:
Periodico
Settore Disciplinare:
Physical, Chemical & Earth Sciences
Citazioni:
44
Recensione:
Indirizzi per estratti:
Indirizzo: Holdaway, MJ 855 Elliott St, Longmont, CO 80501 USA 855 Elliott St Longmont CO USA 80501 Longmont, CO 80501 USA
Citazione:
M.J. Holdaway, "Recalibration of the GASP geobarometer in light of recent garnet and plagioclase activity models and versions of the garnet-biotite geothermometer", AM MINERAL, 86(10), 2001, pp. 1117-1129

Abstract

The garnet-Al silicate-plagioclase (GASP) geobarometer has been recalibrated using four recent garnet activity models, four analogous garnet-biotite temperature models, and two recent plagioclase. activity models. A typical sillimanite-bearing sample that formed at about 5.25 kbar, 575 degreesC shows a possible P range of similar to0.7 kbar due to T error, similar to1 kbar due to range of garnet activity model, similar to0.9 kbar due to range ofplagioclase activity model, and similar to5.4 kbar due to range. of experimental end-member reversals extended by one sigma. Calibrations were further constrained with the kyanite-sillimanite (K-S) phase boundary such that the best fit of 76 pelitic schist samples from 11 localities provides an individual end-member calibration for each of the eight possible combinations of garnet and plagioclase. activity models with the appropriate geothermometer. Samples with low grossular or anorthite component were rejected. The end-member calibrations are constrained to pass through the the best-determined portion of the GASP experimental reversals at 1230 degreesC, 26.6 kbar. These individual end-member calibrations provide self-consistent models that tend to compensate for error in the garnet and plagioclase activity expressions. The models were also tested on a set of 59 samples from the Alps. The recommended calibration is the average garnet activity model and average garnet-biotite T model of Holdaway (2000), the Fuhrman and Lindsley (1988) plagioclase activity model, and H-Grs = -6628521, S-Grs = 258.76 to combine with the remaining phases in the Berman database to produce the optimumend-member GASP curve. These thermodynamic data are for the GASP geobarometer only. Error is about +/-0.8 kbar absolute and about +/-0.6 kbar relative. Geological error is the largest component of error in many of these samples. Care should be taken to be sure that analyzed plagioclase and biotite are near analyzed garnet, that the peak-T portions of garnet and plagioclase are selected, that the peak-T Al silicate is determined, and that the T calculated is the most accurate possible. These calibrations represent an improvement over previous published GASP calibrations. These eight models areavailable for distribution as three programs (T, P, P-T intersection) for the DOS-based personal computer.

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Documento generato il 07/07/20 alle ore 15:19:06