Results 71 to 80 of about 802 (132)
Comparaison géochimique des chromites d'Andorinha et de Campo-Formoso, Bahia (Brésil) [PDF]
Novikoff, André +1 more
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Bazoljubno borovje v Sloveniji : združbe črnega in rdečega bora na karbonatni podlagi in rušja v alpskih dolinah [PDF]
Dakskobler, Igor +2 more
core
Weekly reports for R.V. Polarstern expedition PS100 (2016-07-18 - 2016-09-06, Tromsø - Tromsø), German and English version [PDF]
Kanzow, Torsten
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Electrical Resistivity of Dehydrating Serpentinite
David Bruhn +2 more
openaire +2 more sources
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Feddes Repertorium, 1984
Vom Serpentinit im Slavkovský les (Kaiserwald) bei Mariánské lázně (Marienbad) in Westböhmen werden vier Gesellschaften beschrieben. Den Mittelpunkt unserer Bemühungen stellt das Asplenietum serpentini Gauckl.
W. Müller‐Stoll, M. Toman
exaly +2 more sources
Vom Serpentinit im Slavkovský les (Kaiserwald) bei Mariánské lázně (Marienbad) in Westböhmen werden vier Gesellschaften beschrieben. Den Mittelpunkt unserer Bemühungen stellt das Asplenietum serpentini Gauckl.
W. Müller‐Stoll, M. Toman
exaly +2 more sources
Flora: Morphology, Distribution, Functional Ecology of Plants, 1978
Heinz Höhne
exaly +2 more sources
Heinz Höhne
exaly +2 more sources
Zeitschrift Fur Pflanzenernahrung Und Bodenkunde = Journal of Plant Nutrition and Plant Science, 1990
M. Kanig, T. Soeprapto, G. Friedrich
exaly +2 more sources
M. Kanig, T. Soeprapto, G. Friedrich
exaly +2 more sources
Geology Today, 2012
Serpentinites are metamorphic rocks formed from the alteration of ultramafic igneous rocks. Their precursors largely consist of clinopyroxene, orthopyroxene, olivine and a member of the spinel group, along with other accessory minerals. Serpentinization can be produced through the percolation of fluids of different origins.
Dolores Pereira, Mercedes Peinado
openaire +1 more source
Serpentinites are metamorphic rocks formed from the alteration of ultramafic igneous rocks. Their precursors largely consist of clinopyroxene, orthopyroxene, olivine and a member of the spinel group, along with other accessory minerals. Serpentinization can be produced through the percolation of fluids of different origins.
Dolores Pereira, Mercedes Peinado
openaire +1 more source

