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
.