Zobrazeno 1 - 10
of 38
pro vyhledávání: '"Claude Williamson"'
Publikováno v:
Remote Sensing, Vol 12, Iss 19, p 3123 (2020)
Gossans are surficial deposits that form in host bedrock by the alteration of sulphides by acidic and oxidizing fluids. These deposits are typically a few meters to kilometers in size and they constitute important vectors to buried ore deposits. Hund
Externí odkaz:
https://doaj.org/article/1fad45b1919546f788b748e966a611c1
Publikováno v:
Mineralium Deposita. 57:207-233
Mafic-ultramafic subvolcanic intrusive complexes, at the 1–10-km scale, constitute favorable environments for the formation of orthomagmatic Ni-Cu-PGE sulfide deposits. Within 100–1000-km scale large igneous provinces (LIPs), the most favorable e
Publikováno v:
Geological Magazine. 157:1983-2003
Volcanic rocks from the Davis Strait were studied to elucidate the tectonomagmatic processes during rifting and the start of seafloor spreading, and the formation of the Ungava transform zone between Canada and Greenland. The rocks are from the wells
Enigmatic massive sulphide mineralization in the High Arctic Large Igneous Province, Nunavut, Canada
Publikováno v:
Canadian Journal of Earth Sciences. 56:790-801
Modern mineral exploration strategies should take into account nontraditional metallogenic models for a given geological environment. Here we document the first detailed study of a massive sulphide showing associated with the High Arctic Large Igneou
Located along the Canadian polar continental margin, the Sverdrup Basin is an elongated, intracontinental sedimentary basin that originated during Carboniferous-Early Permian rifting. Starting in the Early Cretaceous, volcanic complexes (VC) were emp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::975366effe58a2b19340cf22e66df375
https://doi.org/10.5194/egusphere-egu21-12230
https://doi.org/10.5194/egusphere-egu21-12230
Publikováno v:
Remote Sensing, Vol 12, Iss 3123, p 3123 (2020)
Remote Sensing; Volume 12; Issue 19; Pages: 3123
Remote Sensing; Volume 12; Issue 19; Pages: 3123
Gossans are surficial deposits that form in host bedrock by the alteration of sulphides by acidic and oxidizing fluids. These deposits are typically a few meters to kilometers in size and they constitute important vectors to buried ore deposits. Hund
Publikováno v:
Geological Society of America Abstracts with Programs.
Publikováno v:
Canadian Journal of Earth Sciences. 53:528-542
The Cretaceous to Paleogene High Arctic Large Igneous Province (HALIP) occurs in circum-Arctic regions, and the largest portion of the province occurs in Canada’s Arctic Archipelago. This paper reviews and documents the geometry and distribution of
Publikováno v:
Applied Clay Science. 119:431-440
Gossans resulting from the oxidation of sulphide-rich bedrock occur sporadically across Canada, and these features are routinely indicated on geological maps published by the Geological Survey of Canada (GSC). In the Canadian Arctic Islands, some gos