Zobrazeno 1 - 10
of 40
pro vyhledávání: '"Takeshi, Imayama"'
Publikováno v:
The Journal of the Geological Society of Japan. 129:307-324
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ba19b95c44c9f5e5ed92a81f49e4a288
https://doi.org/10.5575/geosoc.2022.0061
https://doi.org/10.5575/geosoc.2022.0061
Autor:
Taku, Endo, Takeshi, Imayama
Publikováno v:
フロンティア理工学研究所研究報告 = The bulletin of Research Institute of Frontier Science and Technology. 4:25-28
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=jairo_______::c1e1223a675677ff6c44d34ad1025efb
http://id.nii.ac.jp/1182/00003130/
http://id.nii.ac.jp/1182/00003130/
Autor:
Takeshi Imayama, Akinori Sato, Dripta Dutta, Yasuaki Kaneda, Shota Watanabe, Takeshi Hasegawa, Masayo Minami, Yuki Wakasugi, Shigeyuki Wakaki, Yi Keewook
Early Cretaceous Nidar Ophiolite Complex (NOC, eastern Ladakh) is associated with the north-dipping supra-subduction of the Neo-Tethyan Ocean along the Indus suture zone. The supra-subduction zone ophiolite formed in the forearc setting records the m
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9d99e720f5603cd0937e68b66c5444ff
https://doi.org/10.5194/egusphere-egu23-2981
https://doi.org/10.5194/egusphere-egu23-2981
Autor:
Takeshi, Imayama
Publikováno v:
岡山理科大学古生物学・年代学研究センター事業報告. 2:59-62
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=jairo_______::7c66c18cb6a0f56d9f0c426eb678246b
http://id.nii.ac.jp/1182/00003171/
http://id.nii.ac.jp/1182/00003171/
Publikováno v:
Journal of Metamorphic Geology.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4ec11bfde5438acfa71e0b872365c605
https://doi.org/10.1111/jmg.12718
https://doi.org/10.1111/jmg.12718
Publikováno v:
Journal of Earth System Science. 132
In the Bhagirathi River Transect of the Garhwal Himalaya, India, the existence of the Jhala Normal Fault (JNF) and its movement sense are disputed. The JNF has been considered either as part of the South Tibetan Detachment System (STDS) or as a disti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6e10fcd8125da27ac802d743ebbe677a
https://doi.org/10.1007/s12040-022-02019-4
https://doi.org/10.1007/s12040-022-02019-4
Publikováno v:
フロンティア理工学研究所研究報告 = The bulletin of Research Institute of Frontier Science and Technology. 3:37-41
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=jairo_______::da8fc2075e6d613242935f36ea7b3ac7
http://id.nii.ac.jp/1182/00003111/
http://id.nii.ac.jp/1182/00003111/
Publikováno v:
Journal of Metamorphic Geology. 40:257-286
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::21bdcbefaa2bb88e72bee626f0ee864d
https://doi.org/10.1111/jmg.12627
https://doi.org/10.1111/jmg.12627
Autor:
Toru Nagahashi, Yoshihiro Asahara, Hayato Ueda, Tadashi Usuki, Masayo Minami, Takeshi Imayama
Publikováno v:
Mineralogy and Petrology. 114:305-318
Three types of amphibolites were found around a large serpentinite body in the basement of the Ohmachi Seamount in the Izu-Bonin-Mariana arc: epidote-albite amphibolite, epidote-garnet amphibolite, and garnet-zoisite amphibolite. The epidote-albite a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ad89d11fd1cb1654e9c7586b188783b9
https://doi.org/10.1007/s00710-020-00705-z
https://doi.org/10.1007/s00710-020-00705-z
Publikováno v:
International Journal of Earth Sciences. 109:465-488
The metamorphic pressure–temperature (P–T) conditions across the Main central thrust (MCT) in the Arun area have been investigated. The MCT marks the tectono-metamorphic boundary between the overlying high-grade High Himalaya crystalline sequence
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b92457fc686e0e2620dfd43f1f22b66d
https://doi.org/10.1007/s00531-019-01816-5
https://doi.org/10.1007/s00531-019-01816-5