Works matching IS 00721050 AND DT 2000 AND VI 35 AND IP 3/4
Results: 12
High-Si phengite, mineral chemistry and P-T evolution of ultra-high-pressure eclogites and calc-silicates from the Dabie Shan, eastern China.
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- Geological Journal, 2000, v. 35, n. 3/4, p. 185, doi. 10.1002/gj.863
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Exhumation paths of high-pressure metapelites obtained from local equilibria for chlorite-phengite assemblages.
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- Geological Journal, 2000, v. 35, n. 3/4, p. 139, doi. 10.1002/gj.856
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The southern Menderes Massif (western Turkey): geochronology and exhumation history.
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- Geological Journal, 2000, v. 35, n. 3/4, p. 285, doi. 10.1002/gj.849
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A moderate exhumation rate for the high-pressure Maksyutov Complex, southern Urals, Russia.
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- Geological Journal, 2000, v. 35, n. 3/4, p. 327, doi. 10.1002/gj.862
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High-temperature, low/medium-pressure clockwise P-T paths and melting in the development of regional migmatites: the role of crustal thickening and repeated plutonism.
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- Geological Journal, 2000, v. 35, n. 3/4, p. 345, doi. 10.1002/gj.866
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Exhumation of high-pressure granulites of the Guaxupé Complex, southeastern Brazil.
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- Geological Journal, 2000, v. 35, n. 3/4, p. 231, doi. 10.1002/gj.859
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Neogene exhumation of the Variscan Szeghalom Dome, Pannonian Basin, E. Hungary.
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- Geological Journal, 2000, v. 35, n. 3/4, p. 265, doi. 10.1002/gj.861
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Preface.
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- Geological Journal, 2000, v. 35, n. 3/4, p. 137, doi. 10.1002/gj.865
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Non-silicate inclusions in garnet from an ultra-deep orogenic peridotite.
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- Geological Journal, 2000, v. 35, n. 3/4, p. 209, doi. 10.1002/gj.858
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Structural and petrological constraints on the tectono-metamorphic evolution of the Massa Unit (Alpi Apuane, NW Tuscany, Italy).
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- Geological Journal, 2000, v. 35, n. 3/4, p. 251, doi. 10.1002/gj.860
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Late Devonian subduction and early-orogenic exhumation of eclogite-facies rocks from the Champtoceaux Complex (Variscan belt, France).
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- Geological Journal, 2000, v. 35, n. 3/4, p. 297, doi. 10.1002/gj.864
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Polyphase evolution and reaction sequence of compositional domains in metabasalt: a model based on local chemical equilibrium and metamorphic differentiation.
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- Geological Journal, 2000, v. 35, n. 3/4, p. 163, doi. 10.1002/gj.857
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- Article