Works matching IS 02634929 AND DT 2000 AND VI 18 AND IP 2
Results: 8
Petrological characterization and tectonic significance of retrogressed garnet peridotites, Raobazhai area, North Dabie Complex, east-central China.
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- Journal of Metamorphic Geology, 2000, v. 18, n. 2, p. 181, doi. 10.1046/j.1525-1314.2000.00237.x
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Petrology and P–T evolution of garnet peridotites from central Sulawesi, Indonesia.
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- Journal of Metamorphic Geology, 2000, v. 18, n. 2, p. 193, doi. 10.1046/j.1525-1314.2000.00238.x
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PREFACE Garnet peridotites and ultrahigh-pressure minerals.
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- Journal of Metamorphic Geology, 2000, v. 18, n. 2, p. 121, doi. 10.1046/j.1525-1314.2000.00246.x
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The garnet–clinopyroxene Fe[sup 2+]–Mg geothermometer: an updated calibration.
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- Journal of Metamorphic Geology, 2000, v. 18, n. 2, p. 211, doi. 10.1046/j.1525-1314.2000.00247.x
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Petrochemical constraints for dual origin of garnet peridotites from the Dabie-Sulu UHP terrane, eastern-central China.
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- Journal of Metamorphic Geology, 2000, v. 18, n. 2, p. 149, doi. 10.1046/j.1525-1314.2000.00248.x
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Deep subduction of mantle-derived garnet peridotites from the Su-Lu UHP metamorphic terrane in China.
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- Journal of Metamorphic Geology, 2000, v. 18, n. 2, p. 167, doi. 10.1046/j.1525-1314.2000.00249.x
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A general model for the intrusion and evolution of ‘mantle’ garnet peridotites in high-pressure and ultra-high-pressure metamorphic terranes.
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- Journal of Metamorphic Geology, 2000, v. 18, n. 2, p. 123, doi. 10.1046/j.1525-1314.2000.00250.x
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Super-silicic garnet microstructures from an orogenic garnet peridotite, evidence for an ultra-deep (>6 GPa) origin.
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- Journal of Metamorphic Geology, 2000, v. 18, n. 2, p. 135, doi. 10.1046/j.1525-1314.2000.00251.x
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- Article