Deformation of melt-bearing systemsinsight from in situ grain-scale analogue experiments
Journal of structural geology. Bd. 27. H. 9. 2005 S. 1666 - 1679
Erscheinungsjahr: 2005
ISBN/ISSN: 0191-8141
Publikationstyp: Zeitschriftenaufsatz
Sprache: Englisch
Doi/URN: 10.1016/j.jsg.2005.05.006
| Geprüft: | Bibliothek |
Inhaltszusammenfassung
The deformation behaviour of partially molten rocks was investigated using in situ analogue experiments with norcamphor+ethanol, as well as partially molten KNO3+LiNO3. Three general deformation regimes could be distinguished during bulk pure shear deformation. In regime I, above ca. 8-10 vol.% liquid (melt) fraction ([phi]bulk), deformation is by compaction, distributed granular flow, and grain boundary sliding (GBS). At [phi]bulk
Autoren
Klassifikation
DFG Fachgebiet:
3.31 - Mathematik
DDC Sachgruppe:
Geowissenschaften
