Microstructural and chemical changes associated with cataclasis and frictional melting at shallow crustal levels: the cataclasite-pseudotachylyte connection
- 1 April 1992
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 204 (3-4) , 243-260
- https://doi.org/10.1016/0040-1951(92)90310-3
Abstract
No abstract availableThis publication has 24 references indexed in Scilit:
- Fault structure, wear mechanisms and rupture processes in pseudotachylyte generationPublished by Elsevier ,2003
- Transient discontinuities in ductile shear zonesPublished by Elsevier ,2003
- The nature and significance of pseudotachylite from the Nason terrane, North Cascade Mountains, WashingtonJournal of Structural Geology, 1989
- Frictional melting in landslide-generated frictionites (hyalomylonites) and fault-generated pseudotachylytes-discussionTectonophysics, 1986
- Pseudotachylyte and the development of ultramylonite bands in the Saint-Barthélemy Massif, French PyreneesJournal of Structural Geology, 1982
- Fracture geometry of pseudotachylyte generation zones: a study of shear fractures formed during seismic eventsJournal of Structural Geology, 1981
- Mechanism of frictional fusion in fault zonesJournal of Structural Geology, 1979
- Are pseudotachylites products of fracture or fusion?Geology, 1978
- Partial fusion along the Alpine Fault Zone, New ZealandGSA Bulletin, 1976
- Mylonites from the San Andreas fault zoneAmerican Journal of Science, 1935