Zobrazeno 1 - 10
of 24
pro vyhledávání: '"Monzen Formation"'
Publikováno v:
BULLETIN OF THE GEOLOGICAL SURVEY OF JAPAN. 59:211-224
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4b1d31fb737f5832eac0dd1c81e299ff
https://doi.org/10.9795/bullgsj.59.211
https://doi.org/10.9795/bullgsj.59.211
Autor:
Kenji Shuto, Masayuki Fukase
Publikováno v:
The Journal of the Geological Society of Japan. 106:280-298
男鹿半島西部地域に分布する漸新統門前層中部の火山岩類について, 岩石学的検討を行った.門前層中部の火山岩類は, 9タイプの斑晶鉱物組み合わせをもつ玄武岩～安山岩からなる.これら
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cffe59962ddc2d89e5c9508baed43a0d
https://doi.org/10.5575/geosoc.106.280
https://doi.org/10.5575/geosoc.106.280
Publikováno v:
地質学雑誌. 106(4):280-298
Oligocene volcanic rocks from the middle part of the Monzen Formation in the Oga Peninsula, northeastern Japan consist of lava flows and pyroclastic rocks. These volcanics are composed of basalts and andesites which can be divided into four groups ba
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=jairo_______::aa840a6602e00bd6440da0d982b2e4e2
https://niigata-u.repo.nii.ac.jp/records/3219
https://niigata-u.repo.nii.ac.jp/records/3219
Autor:
Tsoy, I. B.1 (AUTHOR) tsoy@poi.dvo.ru, Vashchenkova, N. G.1 (AUTHOR), Vasilenko, L. N.1 (AUTHOR), Gorovaya, M. T.1 (AUTHOR), Vagina, N. K.1 (AUTHOR), Melnichenko, Yu. I.1 (AUTHOR)
Publikováno v:
Stratigraphy & Geological Correlation. Mar2020, Vol. 28 Issue 2, p202-229. 28p.
Publikováno v:
Stratigraphy & Geological Correlation. Jan2017, Vol. 25 Issue 1, p99-121. 23p.
Publikováno v:
Island Arc; Jan2020, Vol. 29 Issue 1, p1-14, 14p
Publikováno v:
BULLETIN OF THE GEOLOGICAL SURVEY OF JAPAN. 59:255-266
The Oga Peninsula is situated on the Japan Sea side of the NE Japan Arc (Fig. 1). A Cenozoic succession is well exposed along the coast and has been referred to as a type of Cenozoic succession of northern Japan since Huzioka (1959) established the s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::939736ea03a026c4c7b07c925dc8790a
https://doi.org/10.9795/bullgsj.59.255
https://doi.org/10.9795/bullgsj.59.255
Publikováno v:
Journal of the Japanese Association for Petroleum Technology. 72:608-616
The Shinzan Rhyolites are the uppermost part of the Monzen Formation and discordantly cover the Kamo Lavas of the same formation. The volcanic succession from the Kamo Lavas and correlative Kuguriiwa Lavas to the Shinzan Rhyolites has been accepted t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::083478d213372dbf590fa29746a92d03
https://doi.org/10.3720/japt.72.608
https://doi.org/10.3720/japt.72.608
Autor:
Shuto, K., Nohara-Imanaka, R., Sato, M., Takahashi, T., Takazawa, E., Kawabata, H., Takanashi, K., Ban, M., Watanabe, N., Fujibayashi, N.
Publikováno v:
Journal of Petrology; Nov2015, Vol. 56 Issue 11, p2257-2294, 38p
Publikováno v:
Continent-Ocean Interactions Within East Asian Marginal Seas; 2004, p87-108, 22p