Middle Precambrian detrital monazite and zircon from the hida gneiss on Oki-Dogo Island, Japan: their origin and implications for the correlation of basement gneiss of Southwest Japan and Korea-Reference-Cited by-同舟云学术

Middle Precambrian detrital monazite and zircon from the hida gneiss on Oki-Dogo Island, Japan: their origin and implications for the correlation of basement gneiss of Southwest Japan and Korea

Published:1994-08 Issue:3 Volume:235 Page:277-292
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Suzuki Kazuhiro,Adachi Mamoru

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference40 articles.

1. Permian intraformational conglomerate at Kamiaso, Gifu Prefecture, central Japan;Adachi;J. Geol. Soc. Jpn.,1971

2. Pelitic and quartzo-feldspathic gneisses in the Kamiaso conglomerate — a study of Precambrian geology in Japan and East Asia;Adachi;J. Geol. Soc. Jpn.,1973

3. A preliminary note on the age of detrital monazites and zircons from sandstones in the Upper Triassic Nabae Group, Maizuru terrane;Adachi;Mem. Geol. Soc. Jpn.,1992

4. Were Precambrian gneiss clasts in the Kamiaso conglomerate derived from the eastern Korean Peninsula?;Adachi;Bull. Nagoya Univ. Furukawa Mus.,1993

5. Transect of central Japan: from Hida to Shimanto;Adachi,1992

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