Zobrazeno 1 - 10
of 15
pro vyhledávání: '"Mizuki Ishida"'
Autor:
Mitsuki Ogasawara, Junichiro Ohta, Mizuki Ishida, Kentaro Nakamura, Kazutaka Yasukawa, Yasuhiro Kato
The northern part of Hyogo Prefecture in the southwestern Japan is a unique area having a number of large deposits that had produced various metals of industrial importance. For instance, the Nakaze deposit had been known for its extremely high-grade
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::80dfef2bfbb92090415807d28502ee0f
https://doi.org/10.5194/egusphere-egu23-10450
https://doi.org/10.5194/egusphere-egu23-10450
Epithermal deposits are formed in shallow (< 1 km) crustal environments by precipitation of ore minerals from hydrothermal fluids, associated with magmatic activities. Epithermal deposits are important sources of gold and associated critical metals (
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::67efdfc08090651b9b8d01b2776f422b
https://doi.org/10.5194/egusphere-egu23-3728
https://doi.org/10.5194/egusphere-egu23-3728
Autor:
Mizuki Ishida, Takayuki Itoh
Publikováno v:
2022 International Conference on Cyberworlds (CW).
Publikováno v:
Economic Geology.
Better understanding metallogenesis in oceanic crust depends on costly sea-floor drilling projects in areas where metal-bearing deposits, such as sea-floor massive sulfide deposits, are currently forming. In 2018, International Ocean Discovery Progra
Autor:
Kentaro Nakamura, Kazutaka Yasukawa, Fernando Barra, Mizuki Ishida, Rurik Romero, Martin Reich, Yasuhiro Kato, Mathieu Leisen
Publikováno v:
Mineralium Deposita. 57:129-145
Pyrite geochemistry has proven useful for tracking changes in the composition and physico-chemical conditions of hydrothermal fluids in ore-forming environments. Here, we investigated the microtextural features and chemical composition of pyrite, a m
Autor:
Mizuki Ishida, Tatsuo Nozaki, Yutaro Takaya, Junichiro Ohta, Qing Chang, Jun-Ichi Kimura, Kentaro Nakamura, Yasuhiro Kato
The Re–Os isotopic system is a powerful tool for both geochronology and tracing various geochemical processes. Because the Os isotopic ratio (187Os/188Os) distinctly differs between modern seawater (∼1.06) and hydrothermal fluid (∼0.13), the Re
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::14059ab773650da16b0e8983791f88c3
https://doi.org/10.5194/egusphere-egu22-3372
https://doi.org/10.5194/egusphere-egu22-3372
Autor:
Mizuki Ishida
Publikováno v:
Journal of the Sedimentological Society of Japan. 77:115-119
The Re-Os isotope system is an effective tool in geological studies, especially in radiometric dating. Since both Re and Os are highly siderophile and chalcophile elements, they tend to be concentrated in various sulfide minerals. Therefore, the Re-O
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ef5b6778ec1e5ce85a9124eff3ba29d0
https://doi.org/10.5194/egusphere-egu21-1107
https://doi.org/10.5194/egusphere-egu21-1107
Publikováno v:
Goldschmidt2021 abstracts.
Autor:
Yuta Maki, Mizuki Ishida, Taroh Kinoshita, Philippe M. Campeau, Yoshiko Murakami, Akinori Ninomiya, Yoko Takada
Glycosylphosphatidylinositols (GPIs) are glycolipids that anchor many proteins (GPI-APs) on the cell surface. GPI precursor has three mannoses, which in mammalian cells, are all modified by the addition of ethanolamine-phosphate (EthN-P). It is postu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::004d28e55baeafc01e429fd01d8092fb
https://doi.org/10.1101/2020.11.26.399477
https://doi.org/10.1101/2020.11.26.399477