Works matching IS 00107999 AND DT 2013 AND VI 165 AND IP 5
Results: 9
Eight-phase alkali feldspars: low-temperature cryptoperthite, peristerite and multiple replacement reactions in the Klokken intrusion.
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- Contributions to Mineralogy & Petrology, 2013, v. 165, n. 5, p. 931, doi. 10.1007/s00410-012-0842-5
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Major and trace-element composition and pressure-temperature evolution of rock-buffered fluids in low-grade accretionary-wedge metasediments, Central Alps.
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- Contributions to Mineralogy & Petrology, 2013, v. 165, n. 5, p. 981, doi. 10.1007/s00410-012-0844-3
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Geochemical evidence for melting of carbonated peridotite on Santa Maria Island, Azores.
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- Contributions to Mineralogy & Petrology, 2013, v. 165, n. 5, p. 823, doi. 10.1007/s00410-012-0837-2
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Temporal and chemical connections between plutons and ignimbrites from the Mount Princeton magmatic center.
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- Contributions to Mineralogy & Petrology, 2013, v. 165, n. 5, p. 961, doi. 10.1007/s00410-012-0843-4
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Fluid and melt inclusions in the Mesozoic Fangcheng basalt from North China Craton: implications for magma evolution and fluid/melt-peridotite reaction.
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- Contributions to Mineralogy & Petrology, 2013, v. 165, n. 5, p. 885, doi. 10.1007/s00410-012-0840-7
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Intrusion and contamination of high-temperature dunitic magma: the Nordre Bumandsfjord pluton, Seiland, Arctic Norway.
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- Contributions to Mineralogy & Petrology, 2013, v. 165, n. 5, p. 903, doi. 10.1007/s00410-012-0841-6
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Geochronology and geochemistry of leucosomes in the North Dabie Terrane, East China: implication for post-UHPM crustal melting during exhumation.
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- Contributions to Mineralogy & Petrology, 2013, v. 165, n. 5, p. 1009, doi. 10.1007/s00410-012-0845-2
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Radio-colouration of diamond: a spectroscopic study.
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- Contributions to Mineralogy & Petrology, 2013, v. 165, n. 5, p. 843, doi. 10.1007/s00410-012-0838-1
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Effects of experimental reheating of natural basaltic ash at different temperatures and redox conditions.
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- Contributions to Mineralogy & Petrology, 2013, v. 165, n. 5, p. 863, doi. 10.1007/s00410-012-0839-0
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