Quasi-static fault growth and shear fracture energy in granite

Quasi-static fault growth and shear fracture energy in granite

Using a procedure originally developed to locate earthquakes, acoustic emission arrival-time data are inverted to obtain three-dimensional locations of microseisms.

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Nature (London) 1991-03, Vol.350 (6313), p.39-42
Hauptverfasser: Lockner, D. A, Byerlee, J. D, Kuksenko, V, Ponomarev, A, Sidorin, A
Format: Artikel
Sprache:eng
Schlagworte:
Acoustic emission
Acoustics
Earth sciences
Earth, ocean, space
Earthquakes
Exact sciences and technology
Geology
Seismic activity
Sensors
Tectonics. Structural geology. Plate tectonics
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
Beschreibung
Zusammenfassung:Using a procedure originally developed to locate earthquakes, acoustic emission arrival-time data are inverted to obtain three-dimensional locations of microseisms.
ISSN:0028-0836
1476-4687
DOI:10.1038/350039a0