论文信息 - Granite intrusion tectonics induced by fault motion in central Japan

Granite intrusion tectonics induced by fault motion in central Japan

Yuji KANAORI, Kenji YAIRI Department of Geological Sciences, Faculty of General Education, Gifu University, 1-1 Yanagido, Gifu City, Gifu-ken 501-11, Japan Shin-ichi KAWAKAMI Department of Earth and Planetary Science, Faculty of Education, Gifu University, 1-1 Yanagido, Gifu City, Gifu-ken 501-11, Japan and Toru TAKESHITA Department of Earth Sciences, Faculty of Science, Ehime University, 2-5 Bunkyo-cho, Matsuyama City, Ehime-ken 790, Japan (Received October 30, 1989; Accepted March 8, 1990)

Y. Kanaori | S. Kawakami | T. Takeshita | K. Yairi

[1] 大友幸子. Origin of the median tectonic line , 1992 .

[2] E. Geary,et al. Evidence for syntectonic intrusion of plutons in the Bear Mountains fault zone, California , 1989 .

[3] Paul Segall,et al. Development of simple strike-slip fault zones, Mount Abbot quadrangle, Sierra Nevada, California , 1988 .

[4] Jean-Luc Bouchez,et al. Shear criteria in granite and migmatite deformed in the magmatic and solid states , 1988 .

[5] S. Lamb. Tectonic rotations about vertical axes during the last 4 Ma in part of the New Zealand plate-boundary zone , 1988 .

[6] A. Nur,et al. Strike-slip faulting and block rotation in the Lake Mead fault system , 1986 .

[7] J. Jackson,et al. A block model of distributed deformation by faulting , 1986, Journal of the Geological Society.

[8] T. Masuda,et al. Microstructural development of fine-grained quartz aggregates by syntectonic recrystallization , 1981 .

[9] D. Karig. Material Transport within Accretionary Prisms and the "Knocker" Problem , 1980, The Journal of Geology.