Abstract
Two folding events are distinguished in the Kawakami area, Chugoku Zone. The older fold was formed before the sedimentation of the Upper Triassic Nariwa Group (probably Late Permian). The younger fold was formed after the sedimentation of the Nariwa Group (at a time during Late Triassic to Early Cretaceous), and deformed the older structure. The deformation by the older folding is more intense and more important than that by the younger one. -from English summary
| Original language | English |
|---|---|
| Title of host publication | Journal - Geological Society of Japan |
| Pages | 371-377 |
| Number of pages | 7 |
| Volume | 96 |
| Edition | 5 |
| Publication status | Published - 1990 |
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ASJC Scopus subject areas
- Earth and Planetary Sciences(all)
- Environmental Science(all)
Cite this
Structural analysis of folds developed in the Paleozoic and Triassic sequences in Kawakami area, the Okayama Prefecture. / Suzuki, Shigeyuki; Ossaka, J.; Mitsuno, C.
Journal - Geological Society of Japan. Vol. 96 5. ed. 1990. p. 371-377.Research output: Chapter in Book/Report/Conference proceeding › Chapter
}
TY - CHAP
T1 - Structural analysis of folds developed in the Paleozoic and Triassic sequences in Kawakami area, the Okayama Prefecture
AU - Suzuki, Shigeyuki
AU - Ossaka, J.
AU - Mitsuno, C.
PY - 1990
Y1 - 1990
N2 - Two folding events are distinguished in the Kawakami area, Chugoku Zone. The older fold was formed before the sedimentation of the Upper Triassic Nariwa Group (probably Late Permian). The younger fold was formed after the sedimentation of the Nariwa Group (at a time during Late Triassic to Early Cretaceous), and deformed the older structure. The deformation by the older folding is more intense and more important than that by the younger one. -from English summary
AB - Two folding events are distinguished in the Kawakami area, Chugoku Zone. The older fold was formed before the sedimentation of the Upper Triassic Nariwa Group (probably Late Permian). The younger fold was formed after the sedimentation of the Nariwa Group (at a time during Late Triassic to Early Cretaceous), and deformed the older structure. The deformation by the older folding is more intense and more important than that by the younger one. -from English summary
UR - http://www.scopus.com/inward/record.url?scp=0025636901&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=0025636901&partnerID=8YFLogxK
M3 - Chapter
AN - SCOPUS:0025636901
VL - 96
SP - 371
EP - 377
BT - Journal - Geological Society of Japan
ER -