Trace element mobility in mine waters from granitic pegmatite U–Th–REE deposits, Bancroft area, Ontario
| Autor: | Alexandre J. Desbarats, K.E. Venance, Jeanne B. Percival |
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| Rok vydání: | 2016 |
| Předmět: |
Pluton
Geochemistry Trace element chemistry.chemical_element 010501 environmental sciences Uranium 010502 geochemistry & geophysics 01 natural sciences Pollution Igneous rock Allanite chemistry Adit Geochemistry and Petrology Environmental Chemistry Groundwater Pegmatite Geology 0105 earth and related environmental sciences |
| Zdroj: | Applied Geochemistry. 67:153-167 |
| ISSN: | 0883-2927 |
| Popis: | Small, low-grade, granitic pegmatite U–Th–REE deposits are found throughout the Grenville geological province of eastern Canada. Groundwater quality at historical mining properties in the Bancroft area was investigated in order to better understand the mobility of trace elements that may pose health risks if there is renewed development of this class of mineral deposit. Groundwater samples were obtained from diamond drill holes, flowing adits and flooded mine shafts. Uranium occurs almost entirely in the dissolved ( |
| Databáze: | OpenAIRE |
| Externí odkaz: |
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