Abstract
In the first half of the present paper, a brief review on recent field researches in Japan on fractures including joints and minor faults, are dealt with.For applying fracture analysis to the tectonic developments, it is at first necessary to recognize the succession and, if possible, the time of fracturing. From this point of view, an example of the historical changes of tectonic stress field in the Quaternary time, found in south Kanto district by the writer and his collaborators, is shown.
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