... refer to tuffs mentioned and/or sampled in this study: 1) tuff of Wolverine Creek ( Castor et al. 2000 ; Castor and Faulds 2001 ; Faulds et al. 2016 ), 2) Sample NSP171, 3) Sample 17-NLP-01, and 4) Samples 17-NLP-08, 17-NLP-09, and 17-NLP-10. Measured-section locations for the lithofacies associations...

... group is unconformably overlain by Lower Mississippian metaclastic and mafic to felsic metavolcanic rocks of the Wolverine Lake group ( Figs. 1 – 3 ). Metasedimentary rocks of the Lower Permian Money Creek formation are interpreted to unconformably overlie the Wolverine Lake group. Bimodal felsic...

... by northeast-trending lineaments that apparently control the courses of Pelly River and Wolverine Creek ( Fig. 1 , inset B (after Colpron et al. 2007 )). The course of Yukon River above its confluence with the Pelly River parallels the Teslin Fault suggesting that it may be controlled by underlying lineaments...

... unit of light green tuff occurs in the red sandstones of the Preuss just above the Wolverine Canyon member in Wolverine Canyon a few miles southwest. This occurrence is especially noted because identical-appearing tuff occurs in the lower part of the Twin Creek limestone in the area between Montpelier...

... Lakes plutonic suite cut the Grass Lakes group and then are all unconformably overlain by Lower Mississippian metaclastic and mafic to felsic metavolcanic rocks of the Wolverine Lake group (Figures 3 and 4 ). Metasedimentary rocks of the Money Creek formation and metabasalt of the Campbell Range...

... that underlie the Conant Creek Tuff near Heise. Immediately beneath the Conant Creek Tuff in the Heise cliffs is the previously undated tuff of Wolverine Creek (see discussion below, Fig. 8 ). Sanidine from the lower member exposed at Meadow Creek Dugway ( Fig. 1 , locality 13) yielded a weighted mean age...

..., ST + CC = Stikine and Cache Creek Terranes, Wh = Whitehorse, WL = Watson Lake; (rocks) b = blueschist, e = eclogite (Mississippian), E = eclogite (Permian). Fig. 9 Various lithofacies of Wolverine deposit. (A). Footwall shales with felsic tuff along laminae. (B). Massive carbonaceous...

... stratigraphic sections for felsic rocks of the Fire Lake unit in the hanging wall of the Money Creek thrust fault (b), and felsic rocks of the Kudz Ze Kayah unit and Wolverine succession (c). Figures modified from Murphy and Piercey (1999 , 2000 ) and Piercey and Murphy (2000) . Stratigraphically...

...) with the exception of his “Snowdrift anticline” which here has been renamed “Narrows anticline” after the Narrows on Wolverine Creek where the best exposures occur. Fig. 3 —Tectonic map of northern Blackfoot Mountains, south half of Ammon 15-minute quadrangle. Cenozoic mountain-front faults shown as heavy...

...F ig . 6. Comparative stratigraphy of the Wolverine Creek, Red Dog, and Key Creek plates in the Red Dog district, by use of key from Figure 5 . There may be a disconformity beneath the Siksikpuk Formation in the Wolverine Creek plate. The general stratigraphic range of concordant mineralization...

..., northern California) have been determined. Figure 1. (A) Western United States showing distribution of known Lawlor Tuff outcrops from Sarna-Wojcicki et al. (2011) , Wolverine tuff localities mentioned in the text, and the Heise volcanic center (source of Pre-Kilgore outcrops and eruption...

... of Blacktail Creek, Conant Creek, and Wolverine Creek tuffs (Table 1) . The U-Pb ages in most samples are normally distributed and therefore are treated as single populations. Disequilibrium-corrected 206 Pb/ 238 U zircon crystallization ages overlap within uncertainty with 40 Ar/ 39 Ar sanidine eruption...

... part of the Harebell formation on the south side of Wolverine Creek, directly north of Pinyon Peak contains more tuffaceous material than the lower strata. Some of the claystone is light green, fine-grained, with a soapy feel and conchoidal fracture; it is interbedded with olive-drab hard tuff beds...

...., 2001a , b , 2004 , 2006 ; Murphy et al., 2006 ). Fig. 2. Geology of the immediate Wolverine deposit area, showing the locations of different zones of the Wolverine deposit. Geology from Murphy et al. (2006) . The hanging wall of the Money Creek thrust consists of Upper Devonian...

...) suggestion of calling the Salt Lake Formation in Grand Valley the Teewinot Formation is reasonable. Unfortunately, we could not make a direct geochemical correlation between the BEC/L55100/tuff of Wolverine Creek and any tephra in the Granite Mountains area. We use a technique defined by Borchardt et al...

...Stephen J. Piercey; Jan M. Peter; James K. Mortensen; Suzanne Paradis; Donald C. Murphy; Terry L. Tucker Abstract Porphyritic rhyolite sills form an important component of the footwall of the Wolverine volcanogenic massive sulfide (VMS) deposit, Yukon, Canada, and occur proximal to mineralization...

... ; Layton-Matthews et al., 2013 ; McDonald et al., 2018 ), with particular attention paid to the Zn-enriched Wolverine deposit ( Bradshaw et al., 2008 ; Piercey et al., 2008 , 2016 ; Piercey and Kamber, 2019 ). In 2015, an extensive drilling campaign (BMC Minerals Ltd.) further delineated the ABM...

... plate, SD = S. anchoralis-D. latus conodont zone, Wolv. = Wolverine Creek plate; 11, 12, and 15 through 18 are Mamet foraminifer zones. The configuration of the Lisburne Group platform is not yet known in detail, but studies to date suggest that it may have changed in form from east to west...