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BUL 022

Surficial Geology of the Foremost-Cypress Hills Area, Alberta

Cypress Hills Plateau, upland areas, till plain, lacustrine plains, river channels, and canyons. The South Saskatchewan River drains the northern part of the area, and the Milk River drains the southern part. A small internal drainage basin is ... Show Abstract

Westgate, J.A.  1968-01-01

BUL 006

Upper Cretaceous Foraminifera from the Smoky River Area, Alberta

Upper Cretaceous Foraminifera from the Smoky River Area, Alberta The problem of stratigraphic nomenclature within the Smoky River group is reviewed and a new formation name, Puskwaskau, introduced to designate the shales lying between the Bad Heart ... Show Abstract

Wall, J.H.  1960-01-01

BUL 027

Lithostratigraphy of the Uppermost Cretaceous (Lance) and Paleocene Strata of the Alberta Plains

Abstract: In Alberta relatively undisturbed non-marine Cretaceous and Paleocene strata are preserved as a westerly dipping homoclinical wedge of sediment east of the Rocky Mountain Foothills, analogous to the molasse facies bordering the European Alps. This report describes the lithology of the uppermost Cretaceous and Paleocene beds overlying a thick widespread volcanic ashfall (Kneehills Member of the Edmonton Formation) which was deposited 65 million years ago. The post-Kneehills strata of the Alberta Plains are of considerable interest, for during their deposition thick beds of coal were formed, the Rocky Mountains began to emerge and dinosaurs became extinct. The nomenclature of the post-Kneehills strata is revised by placing he lower boundary of the Paskapoo Formation at the top of the Kneehills Member of the Edmonton Formation in central Alberta and by lowering the base of the Ravenscrag Formation to the top of the Battle Formation in southeastern Alberta The redefined Paskapoo and Ravenscrag Formations thus become equivalent to the Willow Creek Formation of southwestern Alberta and now include the Lance equivalent beds and the Cretaceous-Tertiary transition. Evidence ispresented to show that the Porcupine Hills Formation is much more extensive than formerly mapped and that it overlies the Paskapoo Formation in the vicinity of the Bow River. This discovery dates the hrust-folded foothills structures as an intra-Paleocene event. Analysis of the cross stratification in the post-Kneehills strata indicates that a significant change in paleoslope took place between the deposition of the Paskapoo and Porcupine Hills Formations. A shift in the source area from a dominantly volcanic terrain in the interior of British Columbia in late Cretaceous and early Paleocene time to a dominantly sedimentary terrain in northern Montana during late Paleocene time is postulated to account for the change in detrital composition of the sandstones with time. Most of Upper Cretaceous and Paleocene sandstones are subgreywackes r greywackes. Sandstones of the Paskapoo and Ravenscrag Formations are composed of detrital quartz, chert, volcanic and non-volcanic rock fragments, and minor amounts of clastic carbonates. The heavy mineral assemblage is dominated by first-cycle grains of euhedral iotite, zircon, apatite, epidote and hornblende. Most common among a rich and varied series of intergranular authigenic minerals are clay inerals (montmorillonite, chlorite, kaolinite), zeolites (clinoptilolite) and carbonates (calcite). However, the bulk chemical composition of these sandstones is remarkably uniform, the most notable feature being the high alumina content and the predominance of soda over potash. The Porcupine Hills Formation sandstones are composed of detrital quartz, chert, nonvolcanic rock fragments and clastic carbonates. The heavy mineral assemblage is a residual suite of small abraded grains of zircon, tourmaline and apatite. In contrast to the Paskapoo and Ravenscrag Formations, only three common intergranular mineral cements are present; quartz kaolinite and calcite. The bulk chemical composition of the Porcupine Hills Formation sandstone is characterized by a low alumina and high lime contents, and the predominance of potash over soda. Place Keywords 72e 72l 72m 73d 73e 73l 73m 74d 82g 82h 82i 82j 82n 82o 82p 83a 83b 83c 83d 83e 83f 83g 83h 83i 83j 83k 83l 83m 83n 83o 83p 84a 84b 84c 84d alberta canada Theme Keywords alberta plains lithostratigraphy paleocene strata upper cretaceous

Carrigy, M.A.  1971-01-01

BUL 032

Urban Geology of Edmonton

An urban geology study of the Edmonton area was undertaken by the Alberta Research Council in response to the increasing demand for the geological information needed to formulate land use plans based on natural capabilities and limitations of the ... Show Abstract

Kathol, C.P.  McPherson, R.A.  1975-01-01

BUL 044

Cenomanian Microfloras of the Peace River area, northwestern Alberta

The upper Shaftesbury microflora is of early Cenomanian age and reflects an open marine environment of deposition. Morphologically similar angiosperm pollen are known to ake their entrance in strata of middle Cenomanian age in the United ... Show Abstract

Singh, C.  1983-01-01

BUL 024

A Hydrogeological Study of the Three Hills Area, Alberta

Information concerning the geology and groundwater was obtained from eological reports, oil-company records, a water-well survey, and ifteen drilled and tested bore holes, providing an average density of points of various observations of ... Show Abstract

Toth, J.  1968-01-01