Zobrazeno 1 - 10
of 22
pro vyhledávání: '"Takeno, Setsuo"'
Publikováno v:
Japan Review, 1997 Jan 01(8), 193-208.
Externí odkaz:
https://www.jstor.org/stable/25790987
Publikováno v:
Journal of science of the Hiroshima University. Series C, Earth and planetary sciences. 11(1):41-53
By means of transmission electron microscopy (TEM) and the gold-decoration technique, the surface microtopography of day minerals collected from various mode of occurrence were investigated. The clay minerals investigated exclusively exhibit many kin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::b12fbabe42caa4eb33ffe341857f9fe2
http://ir.lib.hiroshima-u.ac.jp/00053161
http://ir.lib.hiroshima-u.ac.jp/00053161
Publikováno v:
Journal of science of the Hiroshima University. Series C, Earth and planetary sciences. 11(1):33-40
Characteristic micro-textures of hematite found commonly in the Liesegang rocks collected from pyrophyllite ore deposits, Shobara district, southwest Japan were investigated. Detailed observations of the Liesegang rocks under the high magnification r
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::66703cae0051b0fe1d8baaac01ab4d10
http://ir.lib.hiroshima-u.ac.jp/00053160
http://ir.lib.hiroshima-u.ac.jp/00053160
Autor:
OGASAHARA, Hiroshi, JIGE, Mayumi, YAMASHITA, Yoshiko, OHKAWA, Makio, KITAGAWA, Ryuji, NAKASHIMA, Akio, TAKENO, Setsuo
Publikováno v:
Journal of science of the Hiroshima University. Series C, Earth and planetary sciences. 11(1):23-32
Spherulitic textures are commonly found in pyrophyllite ore deposits in Shobara district, Hiroshima Prefecture, Japan. Color photographs of the mode of occurrence, hand specimens and characteristic micro-textures are presented. The spherulitic textur
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::68c9375c35c92f3394ebea765ae48a17
http://ir.lib.hiroshima-u.ac.jp/00053159
http://ir.lib.hiroshima-u.ac.jp/00053159
Publikováno v:
Nichibunken Japan review : bulletin of the International Research Center for Japanese Studies. 8:193-208
Some of the natural minerals formed in arid climate give information on the paleo-climate. A microwave spectroscopy of electron spin resonance, (ESR), which detects the concentration of accumulated defects produced by natural radiation, gives the age
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=jairo_______::fad78b88210f6c402edc93513c6c730f
http://id.nii.ac.jp/1368/00000339/
http://id.nii.ac.jp/1368/00000339/
Publikováno v:
Journal of science of the Hiroshima University. Series C, Earth and planetary sciences. 10(3):487-507
This paper deals with smectite collected from the landslide area in the Neogene Kobe Group, southwest Japan. Samples were collected from throughout the region where the Kobe group was distributed. At the Kinkai area, clear outcrops are developed in w
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::935803a06ea236ee7731579fac7764f9
http://ir.lib.hiroshima-u.ac.jp/00053151
http://ir.lib.hiroshima-u.ac.jp/00053151
Publikováno v:
Journal of science of the Hiroshima University. Series C, Earth and planetary sciences. 10(2):333-347
This paper deals with the chemical composition of clay veins found in granitic rocks distributed in Chugoku district with special reference to constituent clay mineral and chemical composition. Clay minerals were collected from clay veins developed i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::723eba6606ecaa3bc652754f09c3e88d
http://ir.lib.hiroshima-u.ac.jp/00053145
http://ir.lib.hiroshima-u.ac.jp/00053145
Liesegang textures are commonly occurred in pyrophyllite ore deposits in Shobara district, Southewest Japan. Color photographs of mode of occurrence, handspecimens and characteristic microtextures are presented. At the Sankin-motoyama outcrop, Lieseg
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::cf1ec73175403fab6cffc8c15ba56041
http://ir.lib.hiroshima-u.ac.jp/00053154
http://ir.lib.hiroshima-u.ac.jp/00053154
The Mt. Cameroon is a large volcanic horst belonging to the majure tectonic line (Cameroon volcanic line). The geographical morphology of the mountain is controlled by regional tectonics. The Mt. Cameroon is consisted of precambrian metamorphic basem
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::a012efd75956cf875ae538d94d431ba0
http://ir.lib.hiroshima-u.ac.jp/00053155
http://ir.lib.hiroshima-u.ac.jp/00053155
Ca-zeolites such as laumontite, stilbite and chabazite were found in the granitic rocks of both magnetite and ilmenite series of late Cretaceous to Tertiary age developed widely in the Chugoku district. These zeolites occur (1) in veins of various sc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::6c17812b3d8c42bf2a37e70b2c9784ee
http://ir.lib.hiroshima-u.ac.jp/00053140
http://ir.lib.hiroshima-u.ac.jp/00053140