Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Shokawa"'
Publikováno v:
Historical Biology. 27:583-594
A longirostrine choristoderan reptile is described from the Early Cretaceous Tetori Group on the basis of an associated specimen from the Kuwajima Formation, Ishikawa Prefecture. This is the first report of Neochoristodera from Japan. However, the br
Autor:
Tomoyuki Ohashi
Publikováno v:
Paleontological Research. 15:185-188
The Tetori Group (Middle Jurassic to Lower Cretaceous) exposed in the Shokawa area of Gifu Prefecture, Japan, is known as a terrestrial vertebrate fossil site. This area has yielded over 1000 microvertebrates, including choristoderes, Shokawa ikoi (E
Autor:
Tsuyoshi Iizuka, Nao Kusuhashi, Takafumi Hirata, Takeshi Handa, Hiroshige Matsuoka, Ai Matsumoto, Masaki Murakami, Takahiro Tagami
Publikováno v:
Island Arc. 15:378-390
The upper Mesozoic Tetori Group contains numerous fossils of plants and marine and non-marine animals. The group has the potential to provide key information to improve our understanding of the Middle Jurassic to Early Cretaceous biota of East Asia.
Publikováno v:
地球科学. 55(6):321-328
The Tetori Group outcropping along the Matsuyamadani in Shokawa Village, is divided into the Akahoke, Mitarai and Otanyama Formations in asccending order. Based on facies analysis, the Akahoke Formation with wave ripples and hummocky cross stratifica
Autor:
Yoji Arakawa
Publikováno v:
Chemical Geology. 85:101-117
Initial 87 Sr 86 Sr ratios, major- and trace-element compositions have been determined for the Late Triassic to Early Jurassic granitic rocks (Funatsu granitic rocks) in the Hida belt, Japan. Six intrusions, which are exposed in a transverse section
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Publikováno v:
Geological data processing. 1979:27-38
Autor:
Yoji Arakawa
Publikováno v:
JOURNAL OF MINERALOGY, PETROLOGY AND ECONOMIC GEOLOGY. 83:374-387
The Sr isotopic compositions were determined for two intrusions of the Funatsu granitic rocks in the northwestern part of the Hida belt. The Utsubo intrusion, a zoned pluton varying from hornblende tonalite to fine-grained biotite granite, gives a we
Autor:
Kumiko Kamiya, Satoru Harayama
Publikováno v:
The Journal of the Geological Society of Japan. 88:249-269_1