1972
DOI: 10.1139/e72-129
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Geology of the Clachnacudainn Salient Near Albert Canyon, British Columbia

Abstract: The nature of the Clachnacudainn Salient of the Shuswap Metamorphic Complex has been investigated in the vicinity of Albert Canyon, British Columbia. A concordant, folded sheet of granodiorite to quartz–diorite gneiss lying between two contrasting panels of metasedimentary rocks is exposed along the Illecillewaet Valley between Albert Canyon and Revelstoke. The lower panel, consisting predominantly of quartzo–feldspathic schist, is exposed in the Woolsey Creek Window in the core of the Lauretta Dome, and in an… Show more

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Cited by 10 publications
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“…The thrust faults commonly follow bedding glide zones that are linked by ramps along which the faults step across the stratigraphic layering; and the thrust Symbols identifying batholiths are as follows: Ba-Battle Mountain; Bu-Bugaboo; By-Bayonne; F-Fry Creek; H-Horsethief Creek; Ka-Kaniksu; Ku-Kuskanax; N-Nelson; W-White Creek. The Valhalla gneiss complex is identified by the symbol V. The information which is compiled and interpreted in this map is taken from maps by : Balkwill, et al (in press a, b); Benvenuto (1978) ;Bielenstein, et al, (1971); Campbell & Loofbourow (1957); Douglas (1951Douglas ( , 1952Douglas ( , 1958Fyles (1964Fyles ( , 1967Fyles & Hewlett (1959); Gilman (1972); Glover (1978); Harrison & Jobin (1963, 1965; Harrison & Schmidt (1971);Henderson (1954);H6y (1977Huntting et al (1961);Johns (1970);Leech (1959Leech ( , 1960; Little (1960); Miller (1974 a-d);Miller et al (1961);Johns (1970); Ollerenshaw (1975Ollerenshaw ( , 1978; Park & Cannon (1943); Price (1962); Price & Mountjoy (1978a-d, 1979 Read & Wheeler (1976); Reesor (1973); Ross (1959); Sears (1979); Simony & Wind (1970); Thompson (1972); Wheeler (1963); Williams (1949); Yates (1964Yates ( , 1...…”
Section: Structure Of the Southern Canadian Rocky Mountainsmentioning
confidence: 99%
“…The thrust faults commonly follow bedding glide zones that are linked by ramps along which the faults step across the stratigraphic layering; and the thrust Symbols identifying batholiths are as follows: Ba-Battle Mountain; Bu-Bugaboo; By-Bayonne; F-Fry Creek; H-Horsethief Creek; Ka-Kaniksu; Ku-Kuskanax; N-Nelson; W-White Creek. The Valhalla gneiss complex is identified by the symbol V. The information which is compiled and interpreted in this map is taken from maps by : Balkwill, et al (in press a, b); Benvenuto (1978) ;Bielenstein, et al, (1971); Campbell & Loofbourow (1957); Douglas (1951Douglas ( , 1952Douglas ( , 1958Fyles (1964Fyles ( , 1967Fyles & Hewlett (1959); Gilman (1972); Glover (1978); Harrison & Jobin (1963, 1965; Harrison & Schmidt (1971);Henderson (1954);H6y (1977Huntting et al (1961);Johns (1970);Leech (1959Leech ( , 1960; Little (1960); Miller (1974 a-d);Miller et al (1961);Johns (1970); Ollerenshaw (1975Ollerenshaw ( , 1978; Park & Cannon (1943); Price (1962); Price & Mountjoy (1978a-d, 1979 Read & Wheeler (1976); Reesor (1973); Ross (1959); Sears (1979); Simony & Wind (1970); Thompson (1972); Wheeler (1963); Williams (1949); Yates (1964Yates ( , 1...…”
Section: Structure Of the Southern Canadian Rocky Mountainsmentioning
confidence: 99%