1-20 OF 88 RESULTS FOR

Cariboo Terrane

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Journal Article
Published: 01 August 1986
Canadian Journal of Earth Sciences (1986) 23 (8): 1047–1061.
... fault from the overlying age-equivalent but stratigraphically and structurally different Cariboo terrane and ( ii ) separated by a system of faults in the general location of the Southern Rocky Mountain Trench from the age-equivalent but stratigraphically and structurally different North American...
Series: DNAG, Geology of North America
Published: 01 January 1993
DOI: 10.1130/DNAG-GNA-D1.272
EISBN: 9780813754482
.... It (Fig. 4F.2, 4F.3) may have been in the area presently occupied by Cariboo Terrane (Struik and Orchard, 1985; Struik, 1986), which lacks Permian strata and may have been partly subaerially exposed during the Permian Period. A marginal basin to the west of Cariboo Terrane (Barkerville Subterrane...
Journal Article
Journal: Economic Geology
Published: 01 January 2016
Economic Geology (2016) 111 (1): 179–198.
...Suzanne Paradis; George J. Simandl; Halley Keevil; Mati Raudsepp Abstract Carbonate-hosted Pb and Zn mineralization in the Quesnel Lake district (Flipper Creek, Dolomite Flats, Main, Gunn, and Que deposits) forms an ~8-km-long belt in metasedimentary and metavolcanic rocks of the Cariboo terrane...
FIGURES | View All (10)
Journal Article
Journal: Economic Geology
Published: 01 September 2016
Economic Geology (2016) 111 (6): 1321–1345.
... geologic setting of the Cariboo Gold District (white dashed outline) in east-central British Columbia, showing main tectonostratigraphic terranes and major lithological packages present (modified from Rhys et al., 2009 ). Areas of known lode gold occurrences are shown in yellow, and significant placer...
FIGURES | View All (13)
Journal Article
Published: 26 June 2002
Canadian Journal of Earth Sciences (2002) 39 (6): 953–970.
... fault (Intra-Quesnellia Fault) may exist that would accommodate the large (>1000 km) displacement required by the models. This fault could occur along the eastern margin of the Quesnellia Terrane and may lie as far east as the western Cariboo Mountains. Despite discrepancies in the magnitude...
FIGURES | View All (12)
Journal Article
Published: 05 July 2011
Canadian Journal of Earth Sciences (2011) 48 (6): 861–869.
...James W. Haggart; Josephine M. Harris; Christine A. Hutton Abstract Mineral and petroleum exploration in the Cariboo-Chilcotin region of British Columbia is hampered by widespread and extensive cover of Pleistocene glacial deposits and Tertiary volcanic successions. Seeing through this geological...
FIGURES
Journal Article
Published: 28 July 2016
Canadian Journal of Earth Sciences (2016) 53 (10): 993–1009.
... throughout a ∼7 km thick tilted section in the Thor-Odin dome and structurally overlying rocks to construct thermochronological histories using existing U–Pb geochronology data with new 40 Ar/ 39 Ar data and to determine the nature of the boundary between the dome and overlying rocks at Cariboo Alp...
FIGURES | View All (7)
Journal Article
Published: 09 June 2011
Canadian Journal of Earth Sciences (2011) 48 (6): 1091–1111.
... of these components. The onset of the last glacial event was initiated by ice advancing westerly and southwesterly into the study area from an alpine source region located in the Cariboo Mountains. As glaciation intensified, ice from the Coast Mountains coalesced with the Cariboo Mountain ice over the Interior...
FIGURES | View All (14)
Image
Regional geologic setting of the <b>Cariboo</b> Gold District (white dashed outlin...
Published: 01 September 2016
Fig. 1 Regional geologic setting of the Cariboo Gold District (white dashed outline) in east-central British Columbia, showing main tectonostratigraphic terranes and major lithological packages present (modified from Rhys et al., 2009 ). Areas of known lode gold occurrences are shown in yellow
Journal Article
Published: 01 August 2013
The Canadian Mineralogist (2013) 51 (4): 501–536.
... of an ophiolitic affinity (Slide Mountain and Cache Creek oceanic terranes). In certain placers in the Tulameen area, the chromian spinel defines a Cr–Fe 3+ trend indicating derivation from the Tulameen Alaskan-type intrusion in the Quesnellia island-arc terrane. Placer deposits in central British Columbia (Manson...
FIGURES | View All (35)
Journal Article
Journal: AAPG Bulletin
Published: 01 January 1959
AAPG Bulletin (1959) 43 (1): 60–100.
...Wm. H. White ABSTRACT The complicated structure of British Columbia is the cumulative result of no less than six major orogenies since the Proterozoic. Using local names to avoid unintended identification with orogenies elsewhere, these are: (1) East Kootenay, pre-Lower Cambrian; (2) Cariboo, post...
FIGURES | View All (14)
Series: GSA Special Papers
Published: 01 January 1995
DOI: 10.1130/SPE299-p159
... This report presents four U/Pb zircon dates from the Kootenay arc and Cariboo Mountains of southeastern British Columbia. When combined with existing biochronological data, two of these dates tightly constrain the age of shortening of the sedimentary basin between the North American continental...
Series: GSA Memoirs
Published: 01 January 1986
DOI: 10.1130/MEM164-p185
... of orthogneiss points lying between 720 and 360 Ma isochrons and paragneiss points showing a similar scatter and spread toward lower ages—is much like that of the Yukon Crystalline Complex and Cariboo-Omineca Belt in Canada; partial lithologic and historical similarity support the hypothesis of a common origin...
Journal Article
Published: 04 July 2011
Canadian Journal of Earth Sciences (2011) 48 (6): 1065–1089.
... on a map of geological terranes. Surveys flown as part of TGI-3 surveys are the Bonaparte Lake West and Bonaparte Lake East surveys, henceforth collectively referred to as the Bonaparte Lake survey (or area). The MPB surveys include the Quesnel, Likely, Cariboo, and Kamloops surveys. In comparison...
FIGURES | View All (16)
Journal Article
Published: 17 June 2003
Canadian Journal of Earth Sciences (2003) 40 (6): 833–852.
...M. Tardy; H. Lapierre; D. Bosch; A. Cadoux; A. Narros; L.C. Struik; P. Brunet Abstract Le terrane de Slide Mountain est constitué de roches sédimentaires siliceuses et détritiques d’âge dévonien à permien dans lesquelles sont intercalés des basaltes et des dolérites. L’ensemble est recoupé par des...
FIGURES | View All (9)
Journal Article
Published: 09 August 2002
Canadian Journal of Earth Sciences (2002) 39 (7): 1143–1167.
... and Cadwallader (including Methow) terranes and link them by late Middle Jurassic time. The early Relay Mountain Group appears to have been a fore-arc basin, possibly along an oblique–convergent margin in the middle unit. The upper unit indicates major changes to a back-arc basin linked to the Ottarasko...
FIGURES | View All (15)
Journal Article
Published: 11 January 2002
Canadian Journal of Earth Sciences (2002) 39 (1): 65–78.
...S.L. Acton; S.L. Acton; P.S. Simony; L.M. Heaman Abstract The character of the Paleozoic basement of Quesnel Terrane and the position of the terrane accretion surface that separates Quesnel and Kootenay terranes from rocks of the ancient North American margin are subjects of debate. To address...
FIGURES | View All (7)
Journal Article
Published: 17 March 2006
Canadian Journal of Earth Sciences (2006) 43 (2): 213–244.
... Cordillera including the Nicola horst, Mount Lytton - Eagle plutonic complex, Cariboo Mountains, and Mica Creek area, may reflect episodic tectonic activity at the plate margin. 1 Present address: Synergy Geological Consulting, #410, 10116-8th Avenue, Edmonton, AB T6E 6V7, Canada. 2 Deceased...
FIGURES | View All (13)
Journal Article
Published: 14 March 2005
Canadian Journal of Earth Sciences (2005) 42 (2): 215–230.
.... The Eocene landscape of the southern Interior Plateau resembled its modern counterpart, with highlands, plains, and deeply incised drainages, except regional drainage was to the north. An anabranching valley system trending west and northwest from Quesnel and Shuswap Highlands, across the Cariboo Plateau...
FIGURES | View All (9)
Journal Article
Published: 11 October 2017
Canadian Journal of Earth Sciences (2018) 55 (1): 84–110.
... northwards by Early Cretaceous deformation and metamorphism (D 2 M 2 ), manifested in a tightening of Jurassic structures, development of more pervasive ductile fabrics, and Barrovian metamorphism. The D 2 M 2 domain is the southerly continuation of the 600 km long Selkirk–Monashee–Cariboo metamorphic belt...
FIGURES | View All (14)