Zobrazeno 1 - 10
of 27
pro vyhledávání: '"Jean S. Cline"'
Publikováno v:
Economic Geology
A significant characteristic distinguishing Carlin-type Au deposits from other Au deposits is the abundance of invisible Au in arsenian pyrite. Gold occurs primarily as ionic Au1+ in arsenian pyrite and is unstable during subsequent thermal events. I
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b2d5f79b28b3826d82c35bff5ab17826
https://doi.org/10.5382/econgeo.4781
https://doi.org/10.5382/econgeo.4781
Autor:
Bill T. Fischer, Jean S. Cline
Publikováno v:
Economic Geology. 115:1137-1150
The 144 zone is a pseudobreccia-hosted, disseminated gold deposit that formed in the middle to late Cambrian Bonanza King dolostone along an unconformity with the underlying early to middle Cambrian Carrara limestone at Bare Mountain, southern Nevada
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::535d8d27106be53bfb9b485b2d2f9fd6
https://doi.org/10.5382/econgeo.4728
https://doi.org/10.5382/econgeo.4728
Autor:
M.A. Auger, Phillip Gopon, Lars N. Hansen, James O. Douglas, Michael P. Moody, Jon Wade, Laurence J. Robb, Jean S. Cline
Carlin-type gold (CTG) mineralization is one the best studied, yet poorly understood gold mineralization styles in the world. These deposits occur predominantly along NW-SE trends in central Nevada and are characterized by cryptic gold mineralization
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::816393052ddfb711d8edc6b87e3574b1
https://doi.org/10.5194/egusphere-egu2020-22303
https://doi.org/10.5194/egusphere-egu2020-22303
Autor:
Yong Xia, Zhuojun Xie, Michael J. Pribil, Jun Yan, Qinping Tan, Zepeng Wang, Alan E. Koenig, Dongtian Wei, Jean S. Cline
Publikováno v:
Economic Geology. 113:1627-1652
The southwest Guizhou Province, China, contains numerous sediment-hosted Au deposits with Au reserves greater than 700 tonnes. To date, the source of ore fluids that formed the Guizhou sediment-hosted Au deposits is controversial, hampering the formu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::84b521437e005388288273aac6504599
https://doi.org/10.5382/econgeo.2018.4607
https://doi.org/10.5382/econgeo.2018.4607
Publikováno v:
Economic Geology. 112:707-740
The Cortez Hills breccia zone, a Nevada Carlin-type gold deposit located in the Cortez district on the Battle Mountain-Eureka trend, formed within a high-grade polylithic breccia, and grades at the center of the breccia zone are locally in excess of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0f67060b944004e66bfabee52db08893
https://doi.org/10.2113/econgeo.112.4.707
https://doi.org/10.2113/econgeo.112.4.707
Autor:
Jon Wade, James O. Douglas, Lars N. Hansen, Laurence J. Robb, Jean S. Cline, M.A. Auger, Michael P. Moody, Philippe Gopon
Publikováno v:
e-Archivo. Repositorio Institucional de la Universidad Carlos III de Madrid
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Carlin-type gold deposits are one of the most important gold mineralization styles in the world. Despite their economic importance and the large volume of work that has been published, there remain crucial questions regarding their metallogenesis. Mu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fab946c8219209da168a62a64d8834c0
http://ora.ox.ac.uk/objects/uuid:
http://ora.ox.ac.uk/objects/uuid:
Publikováno v:
Mineralium Deposita. 52:69-84
The Paiting gold deposit, Guizhou Province, China, has been regarded as a Carlin-type gold deposit by several researchers. Alteration and ore-related minerals from the Paiting deposit were examined, and results were compared with the Cortez Hills Car
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8c31738928882fd273a4233b9afa1211
https://doi.org/10.1007/s00126-016-0647-y
https://doi.org/10.1007/s00126-016-0647-y
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::378234bb7df26f04db52bed302500f8c
https://doi.org/10.1130/abs/2016am-282398
https://doi.org/10.1130/abs/2016am-282398