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SPE 096

Sphalerite and kimberlite indicator minerals in till from the Zama Lake region, northwest Alberta (NTS 84L and 84M)

Canadian Shield rocks, Paleozoic carbonates and quartzite from the Athabasca Basin and the Cordillera. Kimberlite indicator minerals (KIMs) including Cr-pyrope, Cr-diopside and chromite are present in trace amounts (1 to 2 grains in nine ... Show Abstract

Plouffe, A.  Paulen, R.C.  Smith, R.  Kjarsgaard, I.M.  2008-01-08

SPE 087

Chemistry of Kimberlite Indicator Minerals and Sphalerite Derived from Glacial Sediments of Northwest Alberta

Chemistry of Kimberlite Indicator Minerals and Sphalerite Derived from Glacial Sediments of Northwest Alberta Previous AGS and GSC work have reported the presence of kimberlite indicator minerals (KIMs), sphalerite and galena in glacial sediments ... Show Abstract

Plouffe, A.  Paulen, R.C.  Smith, I.R.  Kjarsgaard, I.M.  2007-04-01

INF 132

Kimberlite- Indicator Mineral Results from Reconnaissance Till Sampling in the East Peace River Region (NTS 84C/East), Alberta

Kimberlite- Indicator Mineral Results from Reconnaissance Till Sampling in the East Peace River Region (NTS 84C/East), Alberta Of the 19 samples collected and processed, 14 contain kimberlite-indicator minerals (KIMs) including pyrope, eclogitic ... Show Abstract

Paulen, R.C.  Waight, B.  Kjarsgaard, I.M.  2008-01-03

BUL 026

Some Characteristics and Physical Properties of Alberta Tills

Maps depicting the regional variation in the chemical and mineralogical composition, and physical properties of tills from throughout the plains region of Alberta were prepared by a computer with an attached plotter.The chemical constituents and ... Show Abstract

Bayrock, L.A.  Pawluk, S.  1969-01-01

GEO 2005-10

Quaternary stratigraphy and till geochemistry of the southern Buffalo Head Hills: results of an auger coring program

In 2002, the Alberta Geological Survey cored nine holes near the K4 kimberlite to intersect the near-surface dispersion of kimberlitic material in the till and to document the glacial stratigraphy and drift thickness. Two additional auger holes ... Show Abstract

Fenton, M.M.  Pawlowicz, J.G.  Paulen, R.C.  Prior, G.J.  2006-01-01

GEO 1997-01

Diamond Indicator Mineral Anomaly From Till Sample Site NAT95-134

Diamond Indicator Mineral Anomaly From Till Sample Site NAT95-134 The Alberta Geological Survey is pleased to introduce a new communication vehicle called Geo-Notes. While these publications will not be as extensive as other AGS publications, ... Show Abstract

Fenton, M.M.  Pawlowicz, J.G.  1997-01-01

GEO 1998-01

Diamond Indicator Minerals from Till, Northern Alberta

Diamond Indicator Minerals from Till, Northern Alberta Regional till sampling for geochemistry and diamond indicator minerals has been ongoing in Alberta since 1992, initially as part of the Canada-Alberta Agreement on Mineral Development (MDA) ... Show Abstract

Pawlowicz, J.G.  Dufresne, M.B.  Fenton, M.M.  1998-05-01

GEO 2005-09

Geochemical soil survey over the K4B kimberlite, Buffalo Head Hills, northern Alberta

Multi-element chemical results were obtained for all samples by inductively coupled plasma atomic emission spectroscopy/mass spectrometry (ICP-AES/MS) analyses following aqua regia digestion. Additional results were obtained on the B- and C-horizon ... Show Abstract

Fenton, M.M.  Pawlowicz, J.G.  Prior, G.J.  2006-02-01

ESR 2000-12

Quaternary Geology and Till Geochemistry, Wapiti Map Area (NTS 83L)

Four physiographic regions can be defined: the Wapiti Plains, the Alberta Plateau Benchlands, the Rocky Mountain Foothills, and the Rocky Mountains.The surficial geology is shown on a 1:250 000 scale map, compiled by Andriashek (1983) based on ... Show Abstract

Fenton, M.M.  Pawlowicz, J.G.  2001-09-30

ESR 2005-01

Geochemical Orientation Surveys (Fiscal Year 2000-2001) for Kimberlites in Northern Alberta

Geochemical Orientation Surveys (Fiscal Year 2000-2001) for Kimberlites in Northern Alberta In northern Alberta, indicator mineral analysis may not be effective for detecting kimberlites because kimberlites are decoupled from streams draining ... Show Abstract

Seneshen, D.M.  Grunsky, E.  Rencz, A.  Hall, G.E.M.  Dunn, C.E.  2005-02-01

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