Automated Author ProfileT. Ferbey
T. Ferbey
Current S-Index
Sum of Dataset Indices for all datasets
Average Dataset Index per Dataset
Average Dataset Index per dataset
Total Datasets
Total datasets for this author
Average FAIR Score
Average FAIR Score per dataset
Total Citations
Total citations to the author's datasets
Total Mentions
Total mentions of the author's datasets
S-Index Interpretation
The S-Index (Sharing Index) is a comprehensive metric that represents the cumulative impact of all your datasets. It is calculated as the sum of Dataset Index scores across all your claimed datasets.
What it means:
- A higher S-index indicates greater overall impact of your datasets relative to typical datasets in their fields of research
- The S-Index grows as you add more datasets or as existing datasets gain more citations and mentions
- It provides a single number to track your research data impact over time
Current S-Index: 11.2 (sum of 20 datasets Dataset Index scores)
More information here.
S-Index Over Time
Cumulative Citations Over Time
Cumulative Mentions Over Time
Datasets
The Quesnel terrane in the Interior Plateau of British Columbia, Canada, is highly prospective for locating new porphyry deposits; however, the bedrock in this region is obscured by a nearly continuous blanket of till, making mineral exploration challenging. Located within the Quesnel terrane is the Mount Polley deposit. It is an alkaline, silica-undersaturated, Cu-Au porphyry deposit mined by Imperial Metals Corporation. Eighty-six basal till samples were collected for geochemical and mineralogical analyses in the region of this deposit. Ore elements (Ag, Au and Cu), as well as pathfinder element (Hg and Zn) contents in till reflect detrital glacial dispersal from the Mount Polley deposit. The distribution of anomalous mineral counts of andradite garnet, apatite, chalcopyrite, epidote, jarosite and native gold also reflect glacial dispersal from the deposit. Outcrop-scale ice-flow indicators indicate a dominant ice-flow event to the NW that was preceded by a southwestward glacial advance. The element and mineral signatures of the Mount Polley Cu-Au porphyry deposit are dispersed in sub-glacial surface tills up to 12 km in the down-ice (NW) direction. We demonstrate that till geochemistry and mineralogy can serve for mineral exploration of Cu-Au porphyry mineralization in drift covered areas.
Authors
- S. Hashmi ;
- B.C. Ward ;
- A. Plouffe ;
- M.I. Leybourne ;
- T. Ferbey
The Quesnel terrane in the Interior Plateau of British Columbia, Canada, is highly prospective for locating new porphyry deposits; however, the bedrock in this region is obscured by a nearly continuous blanket of till, making mineral exploration challenging. Located within the Quesnel terrane is the Mount Polley deposit. It is an alkaline, silica-undersaturated, Cu-Au porphyry deposit mined by Imperial Metals Corporation. Eighty-six basal till samples were collected for geochemical and mineralogical analyses in the region of this deposit. Ore elements (Ag, Au and Cu), as well as pathfinder element (Hg and Zn) contents in till reflect detrital glacial dispersal from the Mount Polley deposit. The distribution of anomalous mineral counts of andradite garnet, apatite, chalcopyrite, epidote, jarosite and native gold also reflect glacial dispersal from the deposit. Outcrop-scale ice-flow indicators indicate a dominant ice-flow event to the NW that was preceded by a southwestward glacial advance. The element and mineral signatures of the Mount Polley Cu-Au porphyry deposit are dispersed in sub-glacial surface tills up to 12 km in the down-ice (NW) direction. We demonstrate that till geochemistry and mineralogy can serve for mineral exploration of Cu-Au porphyry mineralization in drift covered areas.
Authors
- S. Hashmi ;
- B.C. Ward ;
- A. Plouffe ;
- M.I. Leybourne ;
- T. Ferbey
Comparisons of pXRF analyses with ICP-AES, ICP-MS and IR analysis.
Authors
- A. Plouffe ;
- T. Ferbey ;
- S. Hashmi ;
- B. C. Ward
Chalcopyrite and epidote content of the 0.25 0.5 mm and >3.2 SG fraction of till from the region of the Woodjam prospect.
Authors
- A. Plouffe ;
- T. Ferbey ;
- S. Hashmi ;
- B. C. Ward
Comparisons of pXRF analyses with ICP-AES, ICP-MS and IR analysis.
Authors
- A. Plouffe ;
- T. Ferbey ;
- S. Hashmi ;
- B. C. Ward
Clay fraction geochemistry (Cu) of till from the region of the Highland Valley Copper deposit.
Authors
- A. Plouffe ;
- T. Ferbey ;
- S. Hashmi ;
- B. C. Ward
Comparisons of pXRF analyses with ICP-AES, ICP-MS and IR analysis.
Authors
- A. Plouffe ;
- T. Ferbey ;
- S. Hashmi ;
- B. C. Ward
Clay fraction geochemistry (Cu) of till from the region of the Gibraltar deposit.
Authors
- A. Plouffe ;
- T. Ferbey ;
- S. Hashmi ;
- B. C. Ward
Comparisons of pXRF analyses with ICP-AES, ICP-MS and IR analysis.
Authors
- A. Plouffe ;
- T. Ferbey ;
- S. Hashmi ;
- B. C. Ward
Chalcopyrite and epidote content of the 0.25 0.5 mm and >3.2 SG fraction of till from the region of the Gibraltar deposit.
Authors
- A. Plouffe ;
- T. Ferbey ;
- S. Hashmi ;
- B. C. Ward