...-Desgagné showing and nearby poorly endowed Hazeur showing and Monster Lake deposit share similar features typical of orogenic systems. The stable isotope compositions of tourmaline and quartz from the Moly-Desgagné–Guercheville fault system also display similar characteristics, such as (1) temperature...

... unidirectional, or downward moving later lake water may have contained a sufficient concentration of B, so as to result in the observed small range of B isotope compositions in the Ca borate zone. Localized isotopic gradients may exist at a scale finer than our sampling in the Cemetery and White Monster deposits...

... changes. Conglomerate and sandstone facies were deposited by low-sinuosity braided streams in the upper braid plain - fan environments. Down-slope changes in facies are preserved in the Summit Creek and Monster formations; they record increased channel sinuosity and, in some cases, meandering streams...

...–1892) subsequently coined the term ‘ Dinosauria ’ ( Owen 1842 , p. 103), he included Megalosaurus within this new category (pp. 103–110), along with two other fossil reptiles then known from deposits in England, Iguanodon and Hylaeosaurus , named in 1825 and 1833, respectively ( Torrens 2012...

... or source of the sulphur or both. Data mainly from rocks not associated with ore deposits is reviewed. The wide range of values in sediments can be attributed to bacterial reduction of sea-water sulphate under various conditions. Basalts give ratios near to the meteorite value, 0% 0 , and in detail relate...

... (MacNamara et al. , 1949; Thode et al. , 1958 ). According to Hunt et al. ( 1954 ) the source beds of the hydrocarbons in the Uinta basin were deposited in an enclosed lake which varied from brackish early in its history to highly saline late in its history ( Fig. 2 ). During Eocene time the lake...

... (Harrison and Thode, 1958b) showed a similar relation. In this latter case, not only did the sulphur of the organic matter have a sulphur isotope ratio similar to the associated pyrite but the hydrocarbon deposits did as well. These results confirm the suggestion of Thode, Dunford, and Monster (1958...

... of the Permian and Jurassic evaporites of Table 5 are similar to those reported by Thode and Monster (1965 , 1967 , 1970 ) and Holser and Kaplan (1966) . Because the Mississippian samples are small veinlets, nodules, and cavity fillings in shale beds (rather than bedded evaporite deposits), are 5 to 10 per...

... when their roots were suddenly plunged into salt water. Beneath the surface of these same estuaries, soil cores revealed layered deposits showing a repeated cycle of slow uplift and rapid submergence. Preliminary age estimates based on radiocarbon dating ( Nelson et al. , 1995 ) and tree-ring studies...

...-scale distances. These units are potentially identifiable on seismic data and are valuable for interwell-scale reservoir modeling. Pinch-out of sand units is characterized in two end-member styles, onlap and infill. Onlap and infill indicate the influence of paleotopography on deposition, reflecting...

...Timothy S. Hayes; Gary P. Landis; Joseph F. Whelan; Robert O. Rye; Richard J. Moscati Abstract Ore formation at the Spar Lake red bed-associated strata-bound Cu deposit took place across a mixing and reaction zone between a hot oxidized metals-transporting brine and a reservoir of “sour” (H 2 S...

..., and the Seattle Fault is now recognized as a substantial hazard to the Seattle urban area. The circa A.D. 900 earthquake caused 7 m of vertical uplift on the southern side, sent massive block landslides tumbling into Lake Washington, and created a tsunami in Puget Sound that left sand deposits on Southern...

.... Because of this, collecting localities are greatly diminished, especially the largest, Pit 11, which was deliberately flooded to create a fishing reserve and cooling lake for a nuclear power station. Nevertheless, study of the Mazon Creek is currently undergoing a revival (e.g. Sallan & Coates 2014...

... that predated the onset of geological exploration, and some had long been inhabited by monsters or fairies. Moreover, antiquaries, fossil hunters, and even tourists shared the established geologists’ interest in the underground. Conceiving of the cave as a many-layered political space, this article argues...

..., lagoonal conditions returned, and the evaporites of the transition zone overlie the Jeribe Formation. In the late late Miocene tectonic activity was relatively low and lagoonal-lake basin depositional environments prevailed. These are represented by thin-bedded, terrigenous, fine sands and clayey...

... ' Cold Lake gas oil +0.259° ± 0.001° +0.239° ± 0 .005 ' Athabasca gas oil +0.217° ± 0 .005° -x0 .242° + 0 .008 ' Athabasca total bitumen +0.314° ± 0.002° +0.335' ± 0 .004° It can be seen that the optical activity of the saturated hydrocarbon s from the gas oils of the Medicine River oil is the lowest...

... as great as −25.6 ‰ for gypsum and −25.8 ‰ for sulfur have been measured. Figure 3 — δ 34 S values (CDT) of various deposits in the Delaware basin and Guadalupe Mountains. Values of gypsum and anhydrite from the Castile Formation, Delaware basin, Thode and Monster (1965 ), Holser and Kaplan (1966...

... to Pleistocene units. MACKENZIE ANDERSON- HORTON PLAINS WEST PEEL TROUGH EAST GREAT BASIN EAR Oz ~ '~ ig i Modern delta River and lake )osits Glacial deposits NUKTAK CZI]] [I D D ,4 ?BEAUFORT MACKENZIE BAY 13 KUGMALLIT 12 i - RICHARDS 1 1 REINDEER 1 O MASON RIVEF EAST FORK SMOKING _~ ~ HILLS B - \ [ TREVOR -AI...

... to be alluvial sands and the upper to be river flood plain, swamp an d lake deposits, He postulates that removal of evaporites in the underly- ing Devonian Elk Point beds caused subsidence in the McMurray area . As the area sank, a series of lakes and swamps developed, character- ized by claystones and coaly...