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This thesis is based on the following papers, which will be referred to in the
text by their Roman numerals I - IV.
- Orientation and magnitude of in situ stress to 6.5 km depth in the
Baltic Shield.
B. Lund and M.D. Zoback, Int. J. Rock. Mech. Min. Sci., 36,
169-190, 1999.
- Stress tensor inversion using detailed microearthquake information and
stability constraints: Application to Ölfus in southwest Iceland.
B. Lund and R. Slunga, J. Geophys. Res., 104, 14,947-14,964,
1999.
- Correlation of microearthquake body-wave spectral amplitudes.
B. Lund and R. Böðvarsson, submitted to Bull. Seismol. Soc. Am.,
1999.
- Spectral amplitude grouping and the state of stress: A study of
microearthquake activity before the November 13, 1998, magnitude 5.0
earthquake in Ölfus, Iceland.
B. Lund, R. Slunga and R. Böðvarsson, manuscript.
Papers written during my time at the Department of Earth Sciences
but not included in this thesis:
- Comment on ``Using borehole breakouts to constrain the
complete stress tensor: Results from the Siljan Deep Drilling Project Project
and offshore Santa Maria Basin, California'' by Blair J. Zajac and Joann M.
Stock.
B. Lund and C. Juhlin, J. Geophys. Res., accepted 1999.
- Estimates of current Icelandic stress tensors from the inversion of
microearthquake fault plane solutions.
B. Lund, R. Slunga and R. Böðvarsson, GFF, 118, A95, 1996.
Reprints were made with kind permissions from Elsevier Science (I) and
the American Geophysical Union (II).
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Bjorn Lund
2000-06-14