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SPE 061

Phases 1 to 4 Extech Study of the Early Proterozoic Athabasca Group, Northeastern Alberta

Fifty-five diamond drillholes (DDH) within the Alberta portion of the Athabasca Basin were reviewed.The Athabasca Group is subdivided into six formations within Alberta, which are, from base to top, the Fair Point, Manitou Falls, Lazenby Lake, ... Show Abstract

Ramaekers, P.  2003-12-01

SPE 062

Development, Stratigraphy and Summary Diagenetic History of the Athabasca Basin, Early Proterozoic of Alberta and Its Relation to Uranium Potential

The Athabasca Group in Alberta was deposited between 1730 Ma and 1600 Ma in four sequences, separated by unconformities, and largely deposited in separate sub-basins, in a tectonic environment dominated by regional compressive ... Show Abstract

Ramaekers, P.  2004-01-01

MAP 537

Precambrian Geology of Northeastern Alberta (NTS 74M, 74L and part of 74E)

Between 1994 and 2000, the Geological Survey of Canada remapped a large portion of the Alberta shield at 1:50,000 scale and published the results as preliminary 'open file' and 'A series' maps. The legend displays samarium-neodymium ... Show Abstract

Pana, D.I.  2012-01-12

ESR 2003-01

Stratigraphy and sedimentology of the Athabasca Group in the Net Lake-Maybelle River area, northeastern Alberta

Deposition of the Fair Point Formation commenced with shallow lacustrine sedimentation in fault-controlled paleovalleys that were subsequently infilled with locally derived pebble conglomerate. The overlying Manitou Falls Formation consists of a ... Show Abstract

Post, Ryan  2004-12-01

ESR 2004-01

Sequence stratigraphy and its use for uranium exploration in the western Athabasca Basin of Alberta and Saskatchewan

[...]the overlying Lower and Upper Wolverine Point sequences were probably more widespread beyond the present-day margins of the Athabasca Basin. The uppermost Locker Lake-Otherside sequence, although not complete, represents a late normal ... Show Abstract

Collier, B.  2005-05-01

ESR 2007-10

Sandstone-Hosted Uranium Potential of Southern Alberta Preliminary Assessment

Sandstone-hosted uranium, the past and present exploration model, is a type of deposit that hosts 30 per cent of world uranium reserves (International Atomic Energy Agency, 2003). The geological setting of southern Alberta has much in common with ... Show Abstract

Matveeva, T.M.  Anderson, S.D.A.  2007-11-01

ESR 2004-02

Preliminary Surficial Lineaments Mapping for the Maybelle River Area, Northeast Alberta, Using Remote Sensing Data

Preliminary Surficial Lineaments Mapping for the Maybelle River Area, Northeast Alberta, Using Remote Sensing Data The RADARSAT-1 images acquired by the Alberta Geological Survey (AGS) are from different incidence angles and look directions; ... Show Abstract

Mei, S.  Pana, D.I.  Fenton, M.M.  Olson, R.A.  2005-05-01

ESR 2007-08

Preliminary Water Well Sampling to Assess the Uranium Potential in the Whiskey Gap Area of Southern Alberta (NTS 82H/2, 3)

Within the past two years mineral exploration industry reports have stated that selected well waters in the Milk River Ridge-Whiskey Gap region produced water samples with highly elevated concentrations of radon and, to a lesser extent, ... Show Abstract

Olson, R.A.  Anderson, S.D.A.  2007-07-01

ESR 2006-02

Geological Reconnaissance Work in the Andrew Lake Area of Northeastern Alberta

Selected geological traverses and uranium prospecting, using a sensitive GR130 spectrometer and two STRAT SPP2N scintillometers, were carried on over the main lithological units and more focused around selected radioactive sites previously ... Show Abstract

Pana, D.I.  Olson, R.A.  Byron, S.J.  2006-03-01

OFR 2009-19

Overview of Uranium Exploration Work along the Northern Rim of the Athabasca Basin, Northeastern Alberta

Extensive uranium exploration work in the 1970s, including scintillometer prospecting traverses, geological mapping, airborne and ground geophysics, and drilling, have documented several uraniferous outcrops with 10 000 counts per second, and ... Show Abstract

Pana, D.I.  Olson, R.A.  2009-10-26