PCM
Ultramafische Gesteine

UB-N-NP

Serpentinites are formed during subduction of oceanic crust and can give insights to processes occurring, when the crust meets the mantle.
Pulverpresstabletten
matrix angepasst
nano-partikulär
ultrahomogen
extrem rein
ohne Bindemittel
Klassifizierung
Processed Material
Kategorie
Ultramafische Gesteine
Standort
Col de Bagenelles
Matrix
Serpentinite
Zugewiesene Werte
Major elements, Trace elements
Anwendungsgebiete
Igneous Petrology, Bulk Geochemistry
Geeignet für
Dateien
Produktinformationsblatt

Ultramafische Gesteine

Ultramafic rocks are characterised by very low silica (SiO2) content of <45 m/m%. and low potassium. Their principal mineralogy is comprised of Mg and Fe-rich minerals such as pyroxenes and olivine. The Earth's mantle consists of ultramafic rocks. Another term used to describe these rocks is ultrabasic, which includes rocks, that have a low silica content, but are not high in Mg and Fe i.e. carbonatites and ultrapotassic igneous rocks.