The Tsuiji group is situated in the southern part of the Chichibu terrain in Shima Peninsula, Mie Prefecture. The northern border of the group is in contact with the Imaura group (=Torinosu group) in fault. The southern border of the group is cut by the Butsuzo line and comes into contact with the Matoya group in the Shimanto terrain. It is composed mostly of sandstone and chert with mudstone, alternations of sandstone and mudstone, and schalstein. Several limestone lenses are intercalated in the schallstein. The general trend of the group is ENE-WSW and dips steeply (50°-70°) to the north. The following foraminifer fossils were discovered by the author from a limestone lens at the south-western part of the Aonomine-san, Shima Peninsula. Ya...
1. In the Omi limestone distributed in the Omi-Oyashirazu area, Niigata Prefecture the following fiv...
The Himi Group, of which flora and fauna have been subjected to intensive studies for many years, ha...
Carboniferous and Permian carbonate sequences in Japan are most completely preserved in the Akiyoshi...
We have studied the geology in the Idani district, Shimizu-machi, Aritagun, Wakayama Prefecture, Sou...
The rocks distributed in the so-called Chichibu terrain in the south-central part of Ehime Prefectur...
Permian-Triassic boundary problems in the Tsukumi Limestone, Southern Chichibu Terrane, SW Japan, ha...
The late Early to Middle Permian fusuline faunas of the Akiyoshi Terrane (Permian accretionary compl...
The Sasayama Basin consists of the Taki group of the permian, the Sasayama group of the cretaceous, ...
The Upper Cretaceous Izumi Group consists of extremely thick sedimentary piles. This group in the As...
A Middle Permian brachiopod fauna consisting of seven species in six genera is described from the lo...
The Geology of the Shimanto Belt has been examined in the Miyama area, north of Owase, eastern Kii P...
Yabeina shiraiwensis, Y. yasubaensis and Y. pinguis are synonymous with Neoschwagerina (Sumatrina) m...
Carboniferous and Permian marine faunas in Japan are principally derived from the Akiyoshi Limestone...
There are sediments of Neogene and Quarternary in the Kikaijima Island, Kagoshima prefecture. The ba...
The Chichibu Palaeozoic consists of semi-schists and non-metamorphic rocks, the latter can be separa...
1. In the Omi limestone distributed in the Omi-Oyashirazu area, Niigata Prefecture the following fiv...
The Himi Group, of which flora and fauna have been subjected to intensive studies for many years, ha...
Carboniferous and Permian carbonate sequences in Japan are most completely preserved in the Akiyoshi...
We have studied the geology in the Idani district, Shimizu-machi, Aritagun, Wakayama Prefecture, Sou...
The rocks distributed in the so-called Chichibu terrain in the south-central part of Ehime Prefectur...
Permian-Triassic boundary problems in the Tsukumi Limestone, Southern Chichibu Terrane, SW Japan, ha...
The late Early to Middle Permian fusuline faunas of the Akiyoshi Terrane (Permian accretionary compl...
The Sasayama Basin consists of the Taki group of the permian, the Sasayama group of the cretaceous, ...
The Upper Cretaceous Izumi Group consists of extremely thick sedimentary piles. This group in the As...
A Middle Permian brachiopod fauna consisting of seven species in six genera is described from the lo...
The Geology of the Shimanto Belt has been examined in the Miyama area, north of Owase, eastern Kii P...
Yabeina shiraiwensis, Y. yasubaensis and Y. pinguis are synonymous with Neoschwagerina (Sumatrina) m...
Carboniferous and Permian marine faunas in Japan are principally derived from the Akiyoshi Limestone...
There are sediments of Neogene and Quarternary in the Kikaijima Island, Kagoshima prefecture. The ba...
The Chichibu Palaeozoic consists of semi-schists and non-metamorphic rocks, the latter can be separa...
1. In the Omi limestone distributed in the Omi-Oyashirazu area, Niigata Prefecture the following fiv...
The Himi Group, of which flora and fauna have been subjected to intensive studies for many years, ha...
Carboniferous and Permian carbonate sequences in Japan are most completely preserved in the Akiyoshi...