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1	Ore Petrology and Wallrock Alteration Studies at the Lake Shore Gold Mine, Kirkland Lake, Ontario McInnes, Brent Ian 04 1900 (has links) <p> The Lake Shore Mine has accounted for over a quarter of the gold produced in the Kirkland Lake camp. Petrography suggests that gold is a later phase in the paragenesis of ore minerals. Sulphides precipitated first followed by tellurides and gold. Wallrock alteration adjacent to the quartz veins was studied by thin section and geochemical analysis. Petrography enabled an alteration facies scheme based on predominant alteration minerals to be established. The alteration assemblages suggest the fluid had a high K and CO2 content, low Na, and reduced S content. Geochemical analysis of these samples confirm petrographic observations and suggests major additions of K2O, SiO2, Rb, Sb and Au to the wallrock, and losses of Na2O, Ba and Zr from the wallrock.</p> / Thesis / Bachelor of Science (BSc)
2	Les hauts et les bas de la vie des mineurs de Kirkland Lake (édition 2007) Gaudreau, Guy, Auger, Kevin, Blais, Sophie 05 September 2007 (has links) No description available. Lake Shore Gold Mines Kirkland Lake, Ontario histoire des mineurs du Nord ontarien Wright-Hargreaves Gold Mines
3	A Multidisciplinary Approach for Determining the Extents of the Beds of Complex Natural Lakes in Louisiana Willis, Frank Levins 06 August 2009 (has links) In Louisiana, the beds of natural lakes are owned by the state. The locations of property boundary lines separating state property from private lands have usually been set by determining the levels of natural monuments known as ordinary high water marks. The term is confusing and subjective, leading to controversy in reference to its determination. Catahoula Lake in central Louisiana was chosen as a study site because of its large size, its 20-foot variation in water levels, and its low-relief perimeter. Geology, geomorphology, hydrology, archaeology, vegetation, dendrochronology and dendrohydrology of the ancient cypress fringe, nineteenth century land survey records, historical records, and time-series statistics were applied to determine the elevation range of ordinary high water. Research suggests that the level of the ordinary high water natural monument used universally in Louisiana to define lake boundaries is not the correct natural monument. This research suggests that, for example, the natural monument that defines the Catahoula Lake boundary is not a vertical monument, but rather an areal monument that was originally recognized by nineteenth century U.S. government surveyors and embedded in the evidence extracted from their original field notes. The solution coincides with the boundaries of regional land patents and offers a consistent solution to determining the boundaries of thousands of acres of disputed lands. The procedure is applicable to other lake and swamp boundaries in Louisiana and other states. Lake lake boundary lake shore bed shore bank survey river stream geomorphology geology tree rings cross dating dendrohydrology dendrochronology dendrosedimentology pollenology baldcypress ordinary high water ordinary high water mark Swamplands Act areal cypress fringe alluvial ridge natural monuments cypress knee Great Red River Raft Atchafalaya River raft US General Land Office land survey patent oil and gas litigation

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