Determining P–T paths from garnet zoning using a brute-force computational method

Reconstructing metamorphic pressure–temperature ( P – T ) paths through petrographic textures, mineral assemblages, and compositions is fundamental to the understanding of orogenesis. We present a new method to derive the P – T path of a rock from mineral zoning. Using Perple_X (Connolly in Earth Pl...

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Veröffentlicht in:	Contributions to mineralogy and petrology 2014-04, Vol.167 (4), p.1, Article 997
Hauptverfasser:	Vrijmoed, J. C., Hacker, B. R.
Format:	Artikel
Sprache:	eng
Schlagworte:	Analysis Earth and Environmental Science Earth Sciences Geology Metamorphic rocks Methods Mineral Resources Mineralogy Minerals Original Paper Petrology Rocks Temperature effects Thermodynamics Zoning
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