Abstract
Shima Peninsula occupies the E end of the Kii Peninsula, SW Japan. There, the Chichibu terrain, composed mainly of the late Paleozoic to middle Mesozoic Chichibu Complex, is divided into the northern, middle and southern subbelts by longitudinal faults. Each subbelt trends ENE-WSW. A serpentinite belt called the Gokasho-Arashima Tectonic Line (G-A Line) runs through the middle subbelt in the NE-SW, direction namely slightly oblique to the general trend of this subbelt. Many longitudinal faults, mostly accompanied by thin belts or lenses of serpentinite, branch off from the G-A Line into the SE side. They dissect the Chichibu Complex and the lower Cretaceous cover into numerous tectonic slices separated or partly enclosed by serpentinite. No such faults extend into the NW side. Based on the mode of occurrence of serpentinite at the western terminal of the G-A Line, the possible western extension of this line is suggested.-from English summary
| Original language | English |
|---|---|
| Title of host publication | Journal - Geological Society of Japan |
| Pages | 19-34 |
| Number of pages | 16 |
| Volume | 94 |
| Edition | 1 |
| Publication status | Published - 1988 |
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ASJC Scopus subject areas
- Earth and Planetary Sciences(all)
- Environmental Science(all)
Cite this
Gokasho- Arashima Tectonic Line, as a serpentinite melange zone, in the Shima Peninsula, southwest Japan. / Saka, Y.; Tezuka, S.; Okada, Y.; Ichikawa, M.; Takagi, Hideo.
Journal - Geological Society of Japan. Vol. 94 1. ed. 1988. p. 19-34.Research output: Chapter in Book/Report/Conference proceeding › Chapter
}
TY - CHAP
T1 - Gokasho- Arashima Tectonic Line, as a serpentinite melange zone, in the Shima Peninsula, southwest Japan.
AU - Saka, Y.
AU - Tezuka, S.
AU - Okada, Y.
AU - Ichikawa, M.
AU - Takagi, Hideo
PY - 1988
Y1 - 1988
N2 - Shima Peninsula occupies the E end of the Kii Peninsula, SW Japan. There, the Chichibu terrain, composed mainly of the late Paleozoic to middle Mesozoic Chichibu Complex, is divided into the northern, middle and southern subbelts by longitudinal faults. Each subbelt trends ENE-WSW. A serpentinite belt called the Gokasho-Arashima Tectonic Line (G-A Line) runs through the middle subbelt in the NE-SW, direction namely slightly oblique to the general trend of this subbelt. Many longitudinal faults, mostly accompanied by thin belts or lenses of serpentinite, branch off from the G-A Line into the SE side. They dissect the Chichibu Complex and the lower Cretaceous cover into numerous tectonic slices separated or partly enclosed by serpentinite. No such faults extend into the NW side. Based on the mode of occurrence of serpentinite at the western terminal of the G-A Line, the possible western extension of this line is suggested.-from English summary
AB - Shima Peninsula occupies the E end of the Kii Peninsula, SW Japan. There, the Chichibu terrain, composed mainly of the late Paleozoic to middle Mesozoic Chichibu Complex, is divided into the northern, middle and southern subbelts by longitudinal faults. Each subbelt trends ENE-WSW. A serpentinite belt called the Gokasho-Arashima Tectonic Line (G-A Line) runs through the middle subbelt in the NE-SW, direction namely slightly oblique to the general trend of this subbelt. Many longitudinal faults, mostly accompanied by thin belts or lenses of serpentinite, branch off from the G-A Line into the SE side. They dissect the Chichibu Complex and the lower Cretaceous cover into numerous tectonic slices separated or partly enclosed by serpentinite. No such faults extend into the NW side. Based on the mode of occurrence of serpentinite at the western terminal of the G-A Line, the possible western extension of this line is suggested.-from English summary
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UR - http://www.scopus.com/inward/citedby.url?scp=0023685110&partnerID=8YFLogxK
M3 - Chapter
AN - SCOPUS:0023685110
VL - 94
SP - 19
EP - 34
BT - Journal - Geological Society of Japan
ER -