Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Kaul Gena"'
Publikováno v:
Ecology. 104
Publikováno v:
Asian Journal of Physical and Chemical Sciences. :1-13
Magnetic skarn ore (MSO) is one of the major copper bearing ore extracted by the Ok Tedi Copper Mine in Papua New Guinea (PNG). Copper minerals are recovered by flotation while the iron not associated with copper are discarded as tailings. The object
Autor:
Uta Konno, Miwako Nakaseama, Urumu Tsunogai, Ryohei Suzuki, Hitoshi Chiba, Junichiro Ishibashi, Kaul Gena
Publikováno v:
Resource Geology. 58:267-288
The Yonaguni Knoll IV hydrothermal vent field (24°51′N, 122°42′E) is located at water depths of 1370–1385 m near the western edge of the southern Okinawa Trough. During the YK03–05 and YK04–05 expeditions using the submersible Shinkai 650
Publikováno v:
Resource Geology. 56:183-190
The Onsen site is an active submarine hydrothermal system hosted by the Desmos caldera in the Eastern Manus Basin, Papua New Guinea. The hydrothermal fluid is very acidic (pH=1.5) and abundant native sulfur is deposited around the vent. The δ34S val
Publikováno v:
Resource Geology. 51:31-44
The Onsen acid-sulphate type of mineralization is located in the Desmos caldera, Manus back-arc basin. Hydrothermal precipitates, fresh and altered basaltic andesite collected from the Desmos caldera were studied to determine mineralization and mobil
Autor:
Fumio Inagaki, Kuypers, Marcel M. M., Urumu Tsunogai, Jun-ichiro Ishibashi, Ko-ichi Nakamura, Tina Treude, Satoru Ohkubo, Miwako Nakaseama, Kaul Gena, Hitoshi Chiba, Hisako Hirayama, Takuro Nunoura, Ken Takai, Jørgensen, B. B., Koki Horikoshi, Antje Boetius
Publikováno v:
Inagaki, F, Kuypers, M M M, Tsunogai, U, Ishibashi, J, Nakamura, K, Treude, T, Ohkubo, S, Nakaseama, M, Gena, K, Chiba, H, Hirayama, H, Nunoura, T, Takai, K, Jørgensen, B, Horikoshi, K & Boetius, A 2006, ' Microbial community in a sediment-hosted CO(2) lake of the southern Okinawa Trough hydrothermal system RID C-8303-2011 ', Proceedings of the National Academy of Sciences of the United States of America, vol. 103, no. 38, pp. 14164-14169 .
Aarhus University
Aarhus University
Increasing levels Of CO(2) in the atmosphere are expected to cause climatic change with negative effects on the earth's ecosystems and human society. Consequently, a variety of CO(2) disposal options are discussed, including injection into the deep o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::9810beed8fc1ed2bbbb9a1c142b9ee3a
https://pure.au.dk/portal/da/publications/microbial-community-in-a-sedimenthosted-co2-lake-of-the-southern-okinawa-trough-hydrothermal-system-rid-c83032011(9876bd8c-1433-45d5-bf77-e2d5061166c7).html
https://pure.au.dk/portal/da/publications/microbial-community-in-a-sedimenthosted-co2-lake-of-the-southern-okinawa-trough-hydrothermal-system-rid-c83032011(9876bd8c-1433-45d5-bf77-e2d5061166c7).html
Microbial community in a sediment-hosted CO2 lake of the southern Okinawa Trough hydrothermal system
Autor:
Hitoshi Chiba, Takuro Nunoura, Miwako Nakaseama, Satoru B. Ohkubo, Ken Takai, Bo Barker Jørgensen, Kaul Gena, Marcel M. M. Kuypers, Koki Horikoshi, Fumio Inagaki, Hisako Hirayama, Urumu Tsunogai, Antje Boetius, Tina Treude, Jun-ichiro Ishibashi, Ko-ichi Nakamura
Publikováno v:
Proceedings of the National Academy of Sciences of the United States of America
Increasing levels of CO 2 in the atmosphere are expected to cause climatic change with negative effects on the earth's ecosystems and human society. Consequently, a variety of CO 2 disposal options are discussed, including injection into the deep oce
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a6d6829ad427e8bfa1b495880bfc88fb
https://europepmc.org/articles/PMC1599929/
https://europepmc.org/articles/PMC1599929/
Autor:
Kaul Gena
Publikováno v:
Procedia Earth and Planetary Science, 6 . pp. 226-233.
The Manus back-arc basin host three distinct well known submarine hydrothermal deposits of Vienna Wood, Pacmanus and Onsen sites. The Vienna Wood site is a typical Cu-Zn type of mineralization consisting predominantly of pyrite, marcasite, sphalerite