Zobrazeno 1 - 10
of 20
pro vyhledávání: '"Kazuo Kosaka"'
Publikováno v:
Journal of Geography (Chigaku Zasshi). 124:633-656
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0b6808b53f713d80690ccba2d6b69b95
https://doi.org/10.5026/jgeography.124.633
https://doi.org/10.5026/jgeography.124.633
Autor:
Kazuo Kosaka, Aiming Lin, Takao Miyata, Keiji Takemura, Akihiro Murata, Shin-ichiro Hinoki, Hidemi Tanaka
Publikováno v:
Island Arc. 10:381-391
This paper describes the results of petrographical and meso- to microstructural observations of brittle fault rocks in cores obtained by drilling through the Nojima Fault at a drilling depth of 389.52 m. The zonation of deformation and alteration in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::84991152dd416c082e33e2c3eeee6c24
https://doi.org/10.1111/j.1440-1738.2001.00336.x
https://doi.org/10.1111/j.1440-1738.2001.00336.x
Publikováno v:
Progress in Natural Science. 18:367-373
Since the 1990s, an ultramicro-particle texture in nano- or micron-sized scale has been continually found in shear planes of various rocks, and recently further progress was made in generic physical mechanisms. In this article, the characteristics of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::33b5ecc845c988a58b8788f0a8e96d0d
https://doi.org/10.1016/j.pnsc.2007.12.001
https://doi.org/10.1016/j.pnsc.2007.12.001
Publikováno v:
Science Bulletin. 53:1217-1221
In three shallow-level fault systems in eastern China, nano-sized (30–100 nm) grinding grain textures are found in the thin-shelled rheological layer representing frictional-viscous high strain field. The surface layer near slipping plane is compos
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ba2f34518fecb1eba4d9433e32a01946
https://doi.org/10.1007/s11434-008-0112-0
https://doi.org/10.1007/s11434-008-0112-0
Autor:
Kazuo Kosaka, Tatsuyasu Kawano
Publikováno v:
Journal of the Japan Society of Engineering Geology. 43:124-133
神奈川県鎌倉市にある 「やぐら」 と呼ばれている鎌倉時代の石窟を例に, 塩類風化の季節変化観察と析出物のXRDによる鉱物鑑定を行った. その結果, 析出物は石膏・エプソマイト・テナ
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1e3cd537a26175b94142fefb958c27fc
https://doi.org/10.5110/jjseg.43.124
https://doi.org/10.5110/jjseg.43.124
Autor:
Kazuo Kosaka, Shiro Chikashige
Publikováno v:
The Journal of the Geological Society of Japan. 108:385-393
"跡倉ナップ"の構成地質体のうち埼玉県寄居-小川地域に分布する寄居層,寄居溶結凝灰岩は西南日本内帯起源の異地性岩体であると考えられている.荒川左岸の露頭に見られる寄居層,寄居
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9198fd20ad2badcade09eafb63779ef3
https://doi.org/10.5575/geosoc.108.385
https://doi.org/10.5575/geosoc.108.385
Autor:
Hidemi Tanaka, Shin-Ichiro Hinoki, Kazuo Kosaka, Aiming Lin, Keiji Takemura, Akihiro Murata, Takao Miyata
Publikováno v:
The Island Arc. 10:381-391
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7c300b4598dee39b813b0ec3997b5987
https://doi.org/10.1046/j.1440-1738.2001.00336.x
https://doi.org/10.1046/j.1440-1738.2001.00336.x
K-Ar dating of hydrothermal alteration of the Yorii welded tuffs in the northeastern Kanto Mountains
Autor:
Shiro Chikashige, Kazuo Kosaka
Publikováno v:
The Journal of the Geological Society of Japan. 106:574-577
Yorii welded tuffs in the northeastern Kanto Mountains are penetratively crushed and strongly hydrothermally altered. They are younger constituents of the Atokura Nappe and their ages indicate the lower limit of the time when the Atokura Nappe thrust
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fbdca1565357476d91cf3d4baf23d51a
https://doi.org/10.5575/geosoc.106.574
https://doi.org/10.5575/geosoc.106.574
Publikováno v:
Journal of Structural Geology. 21:1525-1534
Based on microscopic observations of the Miocene Tokuwa granodiorite, central Japan, a method of delineating deformation grades of low-strain granitoids has been derived which utilizes assemblages of elementary deformation textures (EDTs) such as sub
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e85dc844edb82a9255aaa83378bf05d2
https://doi.org/10.1016/s0191-8141(99)00112-1
https://doi.org/10.1016/s0191-8141(99)00112-1
Autor:
Takato Takemura, Kazuo Kosaka
Publikováno v:
Journal of the Japan Society of Engineering Geology. 40:159-165
Microscopic observation of intact granitoids reveals that different kinds of deformation microstructures within mineral grains result from various processes; deformation microstructures due to microcracking, microfaulting, microfolding, recovery and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9254c6ca511b5c96bf037ce710b918e1
https://doi.org/10.5110/jjseg.40.159
https://doi.org/10.5110/jjseg.40.159