RELATIVE MOMENT TENSORS OF THERMALLY-INDUCED MICROCRACKS IN SALT ROCK

Citation
T. Dahm et al., RELATIVE MOMENT TENSORS OF THERMALLY-INDUCED MICROCRACKS IN SALT ROCK, Tectonophysics, 289(1-3), 1998, pp. 61-74
Citations number
15
Categorie Soggetti
Geochemitry & Geophysics
Journal title
ISSN journal
00401951
Volume
289
Issue
1-3
Year of publication
1998
Pages
61 - 74
Database
ISI
SICI code
0040-1951(1998)289:1-3<61:RMTOTM>2.0.ZU;2-F
Abstract
P-wave amplitudes were inverted to obtain relative moment tensors and the corresponding radiation patterns of thermally induced microcracks at 850 m depth in the salt mine Asse near Wolfenbuttel, Germany. Seism ic waves of microcracks that occurred during a 3-week heating experime nt and during the following 12 weeks of cooling were recorded with eig ht high-frequency piezoelectric sensors (5-100 kHz) positioned a few m etres from the sources. About 42,000 microcracking events were automat ically located during this observation period. Two microcrack clusters were studied that occurred immediately after switching off the heater power. The clusters were located a few centimetres from the heater bo rehole. The moment tensors of these clusters indicate dominant shear c racks with a strike-slip radiation pattern. The P-and T-axes direction s appear to coincide with directions of measured maximum and minimum h orizontal stresses. (C) 1998 Elsevier Science B.V. All rights reserved .