...Figure 10. Cathodoluminescence images of dated zircons showing size, shape, and zoning patterns from the Kuna Crest lobe sheeted complex (C49), Kuna Crest lobe unit I (KCL-428), the Waugh Lake pluton (05-183), and the Kuna Crest-Half Dome transitional unit (KCL-536) in the Tuolumne Intrusive...

... ). Zones I, II, and III are the main intrusive units of the KCL; they are separated by gradational contacts ( Fig. 2 ; Memeti et al. 2010 ) and vary mainly in texture, color, and grain size. The southeastern satellite plutons around Waugh Lake and Thousand Island Lake ( Fig. 2 ) are granodioritic...

... by the red dashed line and the Gothic Dome is shown by the purple dashed line. Our thermochronology samples are marked with yellow stars. Eocene paleovalleys are marked with light blue arrows. SWMP—Salida-Waugh Mountain paleovalley; GRP—Gribbles Run paleovalley; TCP—Trout Creek paleovalley; BPP—Buffalo Peaks...

.... Analysis 293 shows that this water has the greatest percentage of secondary salinity of any Embar water sampled in the Big Horn Basin and resembles that at Waugh dome. Black Mountain field .—The Embar formation at Black Mountain has variable porosity and zones of high and low permeability. Its...

... the polytype in a sample is as important as polymorph identification as it can also be used as an ‘indicator mineral’. The geology of the Maritimes Basin was discussed in detail by Papezik and Fong ( 1975 ), Waugh and Urquhart ( 1983 ), and Webb and Roulston ( 1994 ). The Carboniferous (300 m.y...

...Jacek Wachowiak; Adam Pieczka Abstract Pseudocubic crystals of (Fe,Mg,Mn) 3 B 7 O 13 Cl borate, ≤ 1.2 mm in size and yellowish through pale-violet to pale-violet-brown and brownish in color, were found in the Kłodawa salt dome, located within the Mid-Polish Trough (central Poland), an axial part...

.... Both sands contained water, but the well was completed as a small producer from the Curtis sand in the Chugwater redbeds. A well on Waugh dome is listed as an outpost well, because it is 1 4 mile from an abandoned producer. The new well is much higher on structure than earlier wells...

... of New Brunswick. As these deposits were mined or developed, it became evident that they contain a significant concentration of borate minerals. The assemblage of borate minerals was discussed by Roulston & Waugh (1981) for the Penobsquis and Salt Springs (Clover Hill) deposits. F ig . 1...

... (∼190 Ma) is associated with deposition following North Sea rifting and is interpreted to be additionally controlled by North Sea doming (cf. Pharaoh et al., 2010 ). Between rifting events the heat flow decreases to approximately 60 mW/m 2 to attain typical continental heat flow values ( Peisker, 2013...

... ; Arakel, 1986 ), carbonate-cemented alluvial deposits can be 10 km wide and 100 km long. Locally, these deposits may be lensoid or occur as mounds and domes. The carbonate is precipitated mainly in the capillary fringe above the moving groundwater, but also can be precipitated below the water table...

... Subterrex, 701 Waugh Drive. © 1940 American Association of Petroleum Geologists. All rights reserved 1940 American Association of Petroleum Geologists The mining geologist would consider himself seriously handicapped were his interest and study restricted to the geology of an ore deposit...

... Provost C.S. Ki rkwall Lario Frisco Yai rydel l-Bon-Accord Imperial Westl ock ADA Kirkpatr ick Wainoco Haynes (Mikwan) Ceja HB Delburne Hudson's Bay Gilbey West #I Texaco B.A. Sylvan Lake Mobil Willesden Green HB Brazeau River Altana Sundre North Southern Prod. Cdn. At lant ic Ferr ier Dome Caroline...