Zobrazeno 1 - 10
of 16
pro vyhledávání: '"Keiji Kimbara"'
Autor:
Tomiko Nishimura, Keiji Kimbara
Publikováno v:
Journal of the Mineralogical Society of Japan. 15:207-216
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::05b0e5b126694e4d207ef06632154245
https://doi.org/10.2465/gkk1952.15.207
https://doi.org/10.2465/gkk1952.15.207
Autor:
Keiji Kimbara, Hiroshi Nagata
Publikováno v:
The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists. 69:239-254
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e4a3d5f277706b768c11e8e42cb30ee1
https://doi.org/10.2465/ganko1941.69.239
https://doi.org/10.2465/ganko1941.69.239
Autor:
Takahisa Yoshimura, Keiji Kimbara
Publikováno v:
Journal of the Mineralogical Society of Japan. 11:135-142
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1ecea0cc5df8ccbc9925472c11455c98
https://doi.org/10.2465/gkk1952.11.special1_135
https://doi.org/10.2465/gkk1952.11.special1_135
Publikováno v:
The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists. 77:86-93
The hydrothermal rock alteration of the Tamagawa Welded Tuff (1.0 to 2.0 Ma in age) which unconformably covers the Neogene Tertiary sediments is studied to assess the geothermal resources in the Hachimantai geothermal field, northern Japan. The rock
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3d9e71c292fcd3ebb83381c39e4987bd
https://doi.org/10.2465/ganko1941.77.86
https://doi.org/10.2465/ganko1941.77.86
Autor:
Keiji Kimbara, Taiji Ohkubo
Publikováno v:
The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists. 73:125-136
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a49f62096eeea6a9a6eba4acf8c8cb34
https://doi.org/10.2465/ganko1941.73.125
https://doi.org/10.2465/ganko1941.73.125
Autor:
Keiji Kimbara
Publikováno v:
The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists. 78:479-490
Hydrothermal rock alteration in the eastern Hachimantai geothermal area including Toshichi, Matsukawa and Kakkonda, Iwate Prefecture can be divided into two types; alkaline and acidic alteration types. The alkaline alteration type characterized by th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4f0de3861a99edfaadebf6bb0e5400f5
https://doi.org/10.2465/ganko1941.78.479
https://doi.org/10.2465/ganko1941.78.479
Autor:
Keiji Kimbara, Katsuro Ogawa
Publikováno v:
Journal of Geography (Chigaku Zasshi). 92:523-532
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::35e7265b27c01e74bc1a0467734a2915
https://doi.org/10.5026/jgeography.92.7_523
https://doi.org/10.5026/jgeography.92.7_523
Publikováno v:
The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists. 74:433-442
The rock alteration of this area is classified into regional and local ones. The regional alteration consists of montmorillonite and chlorite zones. Considering the distribution and associated mineral paragenesis, it is assumed that the montmorilloni
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::207787d755daed42ade474a9e5bbb8e4
https://doi.org/10.2465/ganko1941.74.433
https://doi.org/10.2465/ganko1941.74.433
Autor:
Toshio Sudo, Keiji Kimbara
Publikováno v:
The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists. 68:246-258
Chloritic clay minerals occur widely in the Miocene tuffaceous sandstone, associated with laumontite, prehnite and epidote. The chloritic minerals are divided into four zones on the basis of the mineral assemblages as follows; Corrensite Zone, Transi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e20a1f1570ed74d3f55d00cc27f3b4eb
https://doi.org/10.2465/ganko1941.68.246
https://doi.org/10.2465/ganko1941.68.246
Publikováno v:
The Journal of the Japanese Association of Mineralogists, Petrologists and Economic Geologists. 66:99-111
An interstratified chlorite-montmorillonite mineral was found as an alteration mineral of tuff and tuffaceous sediments in the Neogene Tertiary “Green Tuff” near the Yamakata-machi, Kuji-Gun, Ibaragi Prefecture. The
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1d6a682b06d3ee977c8997a583345bbf
https://doi.org/10.2465/ganko1941.66.99
https://doi.org/10.2465/ganko1941.66.99