Paleostress orientation from 3-D orientation distribution of microcracks in quartz from the Cretaceous granodiorite core samples drilled through the Nojima Fault, south-west Japan
Author:
Publisher
Wiley
Subject
Geology
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1046/j.1440-1738.2001.00348.x/fullpdf
Reference42 articles.
1. R. W. Allmendinger, 1988 .Stereonet 4.3a(Academic vers.):A Plotting Program for Orientation Data.
2. Geological and geophysical studies of the Nojima Fault from drilling: An outline of the Nojima Fault Zone Probe
3. Determination of the mean principal directions of stresses for a given fault population
4. Inversion of field data in fault tectonics to obtain the regional stress ? I. Single phase fault populations: a new method of computing the stress tensor
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1. Paleostress directions estimated from healed microcracks in the Cretaceous granitoids:;The Journal of the Geological Society of Japan;2017-03-15
2. Fission track and U-Pb zircon ages of psammitic rocks from the Harushinai unit, Kamuikotan metamorphic rocks, central Hokkaido, Japan: constraints on metamorphic histories;Island Arc;2015-11-27
3. Stress rotations and the long-term weakness of the Median Tectonic Line and the Rokko-Awaji Segment;Tectonics;2014-10
4. Paleostress analyses by means of mixed Bingham distributions of healed microcracks in the Ryoke granites, Central Japan;The Journal of the Geological Society of Japan;2014-01-15
5. Estimation of paleostress field from 3-D orientation distribution of microcracks and their geothermal conditions in the Cretaceous granitic rocks in the northern Awaji Island, central Japan;The Journal of the Geological Society of Japan;2012-09-15
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