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pro vyhledávání: '"Kjell P. Skjerlie"'
Autor:
Kjell P. Skjerlie
Publikováno v:
Journal of Petrology. 43:291-314
Fluid-absent melting experiments on a zoisiteand phengite-bearing INTRODUCTION eclogite (omphacite, garnet, quartz, kyanite, zoisite, phengite and Zoisite or clinozoisite is present in many high-pressure rutile) were performed to constrain the meltin
Autor:
Klaus G. Nickel, Thérèse Merle-Méjean, Djamila Bahloul-Hourlier, Yury Gogotsi, Kjell P. Skjerlie, Galina E. Khomenko
Publikováno v:
J. Mater. Chem.. 6:595-604
Interaction of a β-SiC powder with supercritical water has been studied in the temperature range 600–800 °C under 100–500 MPa pressure. Examination of the composition of corrosion products by Raman and IR spectroscopy, XRD, SEM and TEM demonstr
Autor:
A. E. Patiño Douce, Kjell P. Skjerlie
Publikováno v:
Contributions to Mineralogy and Petrology. 122:62-78
We have conducted H2O-undersaturated melting experiments on charges consisting of a layer of a sillimanite-bearing metapelite and a layer of garnet-bearing amphibolite, with the goal of studying how layered metamorphic rocks interact during anatexis.
Autor:
A. Dana Johnston, Kjell P. Skjerlie
Publikováno v:
Journal of Petrology. 34:785-815
Publikováno v:
Contributions to Mineralogy and Petrology. 114:365-378
We report the result of H2O-undersaturated melting experiments on charges consisting of a layer of powdered sillimanite-bearing metapelite (HQ36) and a layer of powdered tonalitic gneiss (AGC150). Experiments were conducted at 10 kbar at 900°, 925°
Autor:
Kjell P. Skjerlie
Publikováno v:
Contributions to Mineralogy and Petrology. 110:473-487
Obduction of the late Ordovician Solund-Stavfjord Ophiolite Complex (443±3 Ma), west Norwegian Caledonides, involved generation and high-level emplacement of granitic and granodioritic dikes and plutons. Initial 87Sr/86Sr ratios in the granites are