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TitreHydro-stratigraphic correlation by portable X-ray fluorescence spectrometry based chemostratigraphy
TéléchargerTéléchargement (publication entière)
AuteurKnight, R D; Kjarsgaard, B A; Russell, H A J; Sharpe, D R
SourceRegional-scale groundwater geoscience in southern Ontario: an Ontario Geological Survey and Geological Survey of Canada groundwater geoscience open house; par Russell, H A J; Priebe, E H; Commission géologique du Canada, Dossier public 8022, 2016 p. 10, https://doi.org/10.4095/297733
Année2016
ÉditeurRessources naturelles Canada
RéunionOntario Geological Survey and Geological Survey of Canada groundwater geoscience open house; Guelph; CA; mars 10, 2016
Documentdossier public
Lang.anglais
DOIhttps://doi.org/10.4095/297733
Mediaen ligne; numérique
Référence reliéeCette publication est contenue dans Russell, H A J; Priebe, E H; (2016). Regional-scale groundwater geoscience in southern Ontario: an Ontario Geological Survey and Geological Survey of Canada groundwater geoscience open house, Commission géologique du Canada, Dossier public 8022
Formatspdf
ProvinceOntario
SNRC30M/05; 40P/08NE; 30M/12; 30M/11NW; 30M/13; 30M/14; 30M/15NW; 30M/15NE; 30M/16NW; 30M/16NE; 31C/04SW; 31C/04NW; 31D/01; 31D/02; 31D/03; 31D/04; 31D/06; 40P/09SE; 40P/09NE; 40P/16SE; 40P/16NE
Lat/Long OENS -80.2500 -77.5000 44.5000 43.2500
Sujetseau souterraine; géochimie des eaux souterraines; ressources en eau souterraine; levés des eaux souterraines; résurgence des eaux souterraines; régimes des eaux souterraines; mouvement des eaux souterraines; niveaux des eaux souterraines; géologie du substratum rocheux; fluorescence aux rayons x; méthodes de fluorescence aux rayons x; Till de Newmarket ; Till d'Halton ; Moraine d'Oak Ridges ; géologie des dépôts meubles/géomorphologie; géochimie; Quaternaire
Consultation
Endroit
 
Bibliothèque de Ressources naturelles Canada - Ottawa (Sciences de la Terre)
 
ProgrammeAquifer Assessment & support to mapping, Géoscience des eaux souterraines
Diffusé2016 03 03
Résumé(disponible en anglais seulement)
In glacial basins stratigraphic correlation is commonly based on lithostratigraphic methods. Correlation can be significantly improved through the use of geophysical and geochemical properties; however widespread subsurface geophysical data is often limited. For groundwater studies, the collection of sediment geochemistry data is often beyond the scope and budget of many programs and is generally not included as a part of routine data collection. Portable X-ray fluorescent (pXRF) spectrometry has proven to be a successful, cost effective tool to characterize the chemostratigraphy of glacially derived sediments and to improve the interpretation of downhole geophysics, micropaleontology results, and pore water geochemistry. Data collected from this method has now become a routine part of borehole studies within the Groundwater Program at the GSC.
Analytical protocols have been developed to utilize portable X-ray fluorescence spectrometry (pXRF) to obtain precise and accurate data for a suit of up to 14 elements detected in the <63 microns grain size fraction (Ba, Ca, Cu, Fe, K, Mn, Ni, Rb, S, Sr, Ti, V, Zn, Zr). This protocol was developed through the analyses of over 10,000 samples obtained from multiple glacial basins across Canada, and verified against traditional laboratory methods (fusion, four acid, aqua regia digestions) using >500 samples.
The introduction of chemostratigraphic techniques to samples collected from boreholes establishes chemical and related mineralogical variations within sediments and contributes to information collected by sediment description, grain size data, downhole geophysical and stratigraphic correlations. Geochemical data also provides an opportunity to establish a chemostratigraphic framework that complements other stratigraphic correlation techniques, for example lithostratigraphy and biostratigraphy.
Results have demonstrated the ability of chemical analyses obtained from pXRF spectrometry to identify stratigraphic units, refine sedimentological interpretations, and correlate within glacial basins. The addition of geochemical analyses has refined paleogeographic interpretations; provenance studies, and provides information to support 3-D geological models with increased confidence in stratigraphic correlations.
A pilot study in the Greater Toronto Area (GTA) of 10 borehole cores, sampled at approximately one metre interval (1057 sample analysis), has provided a proof of concept for planning of a series of chemostratigraphic transects across southern Ontario. Samples will be collected from OGS and GSC archival material for 18-20 boreholes for approximately 2000 samples. Additionally reanalysis of a suite of samples from the NATMAP (< 50 samples) orientation sample transect in the GTA will provide a link with surface geochemical sampling and the subsurface chemostratigraphic data.
GEOSCAN ID297733