Abstract
The Kawai mylonite zone, an inner shear zone of the Ryoke belt, trends N75°E oblique to the general trend (E-W) of the gneissose granites in the Kishiwada area, Osaka Prefecture. Mylonites were formed under sinistral shear movement and cataclasis was overprinted along the Kawai cataclasite zone within the mylonite zone. Mylonites in the northern part of the cataclasite zone are characterized by the occurrence of P-type (higher T and lower δε/δt type) quartz whereas those in the southern part by S-type (lower T and higher δε/δt type) quartz. This contrast suggests that both mylonites were formed under different deformation environment (T and/or δε/δt) and thereafter juxtaposed together during a fault movement along the cataclasite zone. -from English summary
| Original language | English |
|---|---|
| Title of host publication | Journal - Geological Society of Japan |
| Pages | 869-886 |
| Number of pages | 18 |
| Volume | 94 |
| Edition | 11 |
| Publication status | Published - 1988 |
| Externally published | Yes |
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ASJC Scopus subject areas
- Earth and Planetary Sciences(all)
- Environmental Science(all)
Cite this
Deformation of quartz in an inner shear zone of the Ryoke belt : an example in the Kishiwada area, Osaka Prefecture. / Takagi, Hideo; Mizutani, T.; Hiro-Oka, K.
Journal - Geological Society of Japan. Vol. 94 11. ed. 1988. p. 869-886.Research output: Chapter in Book/Report/Conference proceeding › Chapter
}
TY - CHAP
T1 - Deformation of quartz in an inner shear zone of the Ryoke belt
T2 - an example in the Kishiwada area, Osaka Prefecture
AU - Takagi, Hideo
AU - Mizutani, T.
AU - Hiro-Oka, K.
PY - 1988
Y1 - 1988
N2 - The Kawai mylonite zone, an inner shear zone of the Ryoke belt, trends N75°E oblique to the general trend (E-W) of the gneissose granites in the Kishiwada area, Osaka Prefecture. Mylonites were formed under sinistral shear movement and cataclasis was overprinted along the Kawai cataclasite zone within the mylonite zone. Mylonites in the northern part of the cataclasite zone are characterized by the occurrence of P-type (higher T and lower δε/δt type) quartz whereas those in the southern part by S-type (lower T and higher δε/δt type) quartz. This contrast suggests that both mylonites were formed under different deformation environment (T and/or δε/δt) and thereafter juxtaposed together during a fault movement along the cataclasite zone. -from English summary
AB - The Kawai mylonite zone, an inner shear zone of the Ryoke belt, trends N75°E oblique to the general trend (E-W) of the gneissose granites in the Kishiwada area, Osaka Prefecture. Mylonites were formed under sinistral shear movement and cataclasis was overprinted along the Kawai cataclasite zone within the mylonite zone. Mylonites in the northern part of the cataclasite zone are characterized by the occurrence of P-type (higher T and lower δε/δt type) quartz whereas those in the southern part by S-type (lower T and higher δε/δt type) quartz. This contrast suggests that both mylonites were formed under different deformation environment (T and/or δε/δt) and thereafter juxtaposed together during a fault movement along the cataclasite zone. -from English summary
UR - http://www.scopus.com/inward/record.url?scp=0024234116&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=0024234116&partnerID=8YFLogxK
M3 - Chapter
AN - SCOPUS:0024234116
VL - 94
SP - 869
EP - 886
BT - Journal - Geological Society of Japan
ER -