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캐나다
Volcaniclastic gravity flow deposits in the Dezadeash Formation (Jura-Cretaceous), Yukon, Canada: Implications regarding the tectonomagmatic evolution of the Chitina arc in the northern Cordillera of North America
for a copy of this paper please contact the Yukon Geological Survey; geology@gov.yk.ca.
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연관 데이터
An orogenic wedge model for diachronous deformation, metamorphism, and exhumation in the hinterland of the northern Canadian Cordillera
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This paper is available via open access. You can also contact the Yukon Geological Survey (geology@gov.yk.ca) for a copy of this paper.
Late Devonian magmatism and clastic deposition in the upper Earn Group (central Yukon, Canada) mark the transition from passive to active margin along western Laurentia
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for a copy of this paper please contact the Yukon Geological Survey; geology@yukon.ca.
Late Neoproterozoic–early Paleozoic basin evolution in the Coal Creek inlier of Yukon, Canada: implications for the tectonic evolution of northwestern Laurentia
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for a copy of this paper please contact the Yukon Geological Survey; geology@gov.yk.ca.
Tectonic analysis of the Nisling, northern Stikine and northern Cache Creek terranes, Yukon and British Columbia
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A copy of this thesis is available at the EMR library – QE187 J32. This thesis is available online at https://repository.arizona.edu/handle/10150/185864.
Northern Cordillera: Canada and Alaska
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for a copy of this paper please contact the Yukon Geological Survey; geology@gov.yk.ca.
Paleozoic magmatism and crustal recycling along the ancient Pacific margin of North America, northern Cordillera
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for a copy of this paper please contact the Yukon Geological Survey; geology@gov.yk.ca.
Geology of mid-Cretaceous volcanic rocks at Mount Nansen, central Yukon, and their relationship to the Dawson Range batholith
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not_specified
Tectonics and metallogeny of the British Columbia, Yukon and Alaskan Cordillera, 1.8 Ga to the present
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not_specified
2011 Cordilleran Tectonics Workshop Program and Abstracts Volume
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not_specified
Geology of the Dezadeash Range and adjacent northern Coast Mountains (115A), southwestern Yukon: Re-examination of a terrane boundary
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Granodiorite of the Coast Plutonic Complex intruded metasedimentary rocks in the Dezadeash Range of the northern Coast Belt in the late Mesozoic. Graphitic staurolite-biotite schist, associated with the Kluane Metamorphic Assemblage, underlies the western Dezadeash Range, whereas cordierite-biotite gneiss, previously correlated with the Late Proterozoic - Paleozoic Nisling Assemblage, is exposed in the eastern and southern regions. A terrane boundary was placed in the central Dezadeash Range. Recent petrographic studies reveal a southeastward increase in metamorphic grade. Prograde appearance of cordierite partly obliterated an older schistosity and caused a fabric change near the postulated terrane boundary. Furthermore, typical continental margin rocks, such as marble and quartzite, are not observed. This suggests that all metamorphic rocks in the Dezadeash Range can be correlated with the Kluane Metamorphic Assemblage, whereas Nisling Assemblage rocks occur in the Coast Mountains to the east. Therefore, the terrane boundary is located in the Dezadeash River valley, further southeast than previously thought.
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