1-20 OF 144 RESULTS FOR

Teslin Zone

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: 05 June 2001
Canadian Journal of Earth Sciences (2001) 38 (5): 879–882.
... the evolution of the Teslin suture zone (TSZ), previous tectonic models broadly agree that the TSZ comprises a ductile shear zone that constitutes a fundamental crustal boundary (e.g., Tempelman-Kluit 1979 ; Erdmer 1985 ; Hansen 1989 ; Stevens and Erdmer 1996 ; Hansen and Dusel-Bacon 1998 ). In contrast...
Journal Article
Published: 04 June 2001
Canadian Journal of Earth Sciences (2001) 38 (5): 883–887.
... Canada 2001 We reply to the criticisms of Oliver and Hansen on our paper on the structure and tectonic significance of what we prefer to call the Teslin zone (TZ) and Oliver and Hansen the Teslin suture zone (TSZ). They criticize %(% i ) our “scientific methodology,” ( ii ) our interpretation...
FIGURES | View All (5)
Journal Article
Published: 25 August 1999
Canadian Journal of Earth Sciences (1999) 36 (3): 479–494.
...Martin de Keijzer; Paul F Williams; Richard L Brown Abstract The Teslin zone in south-central Yukon has previously been described as a discrete zone with a steep foliation unique to the zone. It includes the Anvil assemblage and the narrowest portion of the Yukon-Tanana terrane (the Nisutlin...
Journal Article
Published: 01 May 1997
Canadian Journal of Earth Sciences (1997) 34 (5): 709–715.
...Robert A. Creaser; Larry M. Heaman; Philippe Erdmer Abstract Zircon from eclogite near Last Peak in the Teslin tectonic zone yielded a U–Pb isotopic age of 269 + 2 Ma (2σ), the first precise age for such a rock in the Yukon –Tanana terrane of the Canadian Cordillera. Both the morphology...
Journal Article
Published: 01 January 1996
Canadian Journal of Earth Sciences (1996) 33 (1): 103–116.
...R. A. Stevens; P. Erdmer; R. A. Creaser; S. L. Grant Abstract Metamorphosed and ductilely deformed sedimentary, plutonic, and volcanic rocks of the Nisutlin and Anvil assemblages make up the Yukon–Tanana terrane in the Teslin tectonic zone study area. The Nisutlin assemblage consists of siliceous...
Journal Article
Published: 01 November 1989
Canadian Journal of Earth Sciences (1989) 26 (11): 2224–2235.
...Vicki L. Hansen; James K. Mortensen; Richard L. Armstrong Abstract The Teslin suture zone (TSZ) comprises a portion of the Yukon–Tanana terrane (YT), in the Yukon, formed by steeply dipping layering and L–S tectonite foliation. The TSZ forms the fundamental tectonic boundary between rocks deposited...
Image
εNd 350  versus  147 Sm/ 144 Sm for felsic rocks from the Finlayson Lake re...
Published: 29 January 2003
Fig. 7. εNd 350 versus 147 Sm/ 144 Sm for felsic rocks from the Finlayson Lake region. Shown for comparison are Nd isotopic data for YTT sedimentary rocks from the Teslin Zone (NI, NII, and NIII from Creaser et al. 1997 ), and unit 1 metasedimentary rocks of the YTT in the Finlayson Lake
Image
(A) Simplified tectonic assemblage map of the northern Canadian Cordillera ...
Published: 24 October 2005
prior to 425 km of post-Late Cretaceous dextral displacement along Tintina fault (Tintina). CR, Campbell Range; CT, Cassiar terrane; JCF, Jules Creek fault; KS, Klondike schist; SA, Sylvester allochthon; SCK, St. Cyr klippe; TFZ, Tummel fault zone; TZ, Teslin zone. Blueschist and eclogite occurrences
Journal Article
Published: 16 September 2005
Canadian Journal of Earth Sciences (2005) 42 (6): 1223–1237.
... that the zone thins in the mid-crust and widens near the Moho. This apparent variable width versus depth of the Tintina fault is atypical of major strike-slip faults worldwide. The Teslin fault was an active terrane boundary during accretion of terranes onto North America. Observed reflection geometries...
FIGURES | View All (11)
Image
The results from the tomography analysis in the area of the <span class="search-highlight">Teslin</span> fault zo...
Published: 16 September 2005
Fig. 11. The results from the tomography analysis in the area of the Teslin fault zone are overlain on a seismic section that was remigrated using a velocity field incorporating the new tomography results. Black arrows indicate surface trace of the Teslin and a parallel fault ( Gordey
Journal Article
Published: 24 October 2005
Canadian Journal of Earth Sciences (2005) 42 (8): 1431–1448.
... prior to 425 km of post-Late Cretaceous dextral displacement along Tintina fault (Tintina). CR, Campbell Range; CT, Cassiar terrane; JCF, Jules Creek fault; KS, Klondike schist; SA, Sylvester allochthon; SCK, St. Cyr klippe; TFZ, Tummel fault zone; TZ, Teslin zone. Blueschist and eclogite occurrences...
FIGURES | View All (8)
Image
Part of the originally processed (migrated) SNORCLE line 3 ( a ) and line 2...
Published: 16 September 2005
Fig. 9. Part of the originally processed (migrated) SNORCLE line 3 ( a ) and line 2a ( b ) sections ( Cook et al. 2004 ) in the area of the Teslin fault zone (Fig.  1 ). In both sections, the lower crust (shaded region) shows no truncations of prominent reflectors and suggests that the faults do
Journal Article
Journal: Geology
Published: 01 January 1992
Geology (1992) 20 (1): 71–74.
...Vicki L. Hansen Abstract Lineated and foliated tectonites of the Teslin suture zone, Yukon, represent the deep-seated part of a west-dipping subduction complex that formed seaward of western North America in Permian-Triassic time. The tectonites were progressively underplated onto the hanging wall...
Journal Article
Journal: GSA Bulletin
Published: 01 January 1985
GSA Bulletin (1985) 96 (1): 1–14.
... the eastern margin of the Intermontane Belt by as much as 300 km. These faults, including the Kutcho and the Pinchi, connect in part with the Teslin Suture Zone in Yukon Territory and probably with the Fraser River-Straight Creek fault zone in southern British Columbia. Although dextral transcurrent faulting...
Journal Article
Published: 02 May 2008
Canadian Journal of Earth Sciences (2008) 45 (3): 389–403.
...; ϵNd T , 4.2 to 1.4), non-subduction-related source identified as the host Cache Creek terrane; and an isotopically slightly more evolved (Sr i , 0.7094 to 0.7101; ϵNd T , 4.5 to –7.3), subduction-related source identified as the host Stikine terrane. Immediately east of the Teslin Tectonic Zone (TTZ...
Journal Article
Published: 01 June 1992
Canadian Journal of Earth Sciences (1992) 29 (6): 1296–1304.
... largely retrograded by postsubduction metamorphism. Their existence is interpreted as additional evidence of the link between nappes above the Cassiar terrane and their inferred root, the Teslin suture zone. The Nisutlin and Anvil allochthonous assemblages can now be interpreted, not simply as crustally...
Journal Article
Published: 01 December 1988
Canadian Journal of Earth Sciences (1988) 25 (12): 2005–2016.
... Columbia; it lies west of the Tintina – Northern Rocky Mountain Trench fault and Teslin Suture Zone and east of the Denali – Shakwak fault. Volcanic sections were sampled in three regions spread over 300 km, providing the first paleomagnetic data from pre-Tertiary volcanic rocks in the northern Canadian...
Image
A location map of the Yukon–Tanana terrane (YTT) in Alaska and western Cana...
Published: 29 July 2002
by the Tintina Fault to the northeast and the Denali Fault to the southwest. The box in the northwestern Yukon–Tanana terrane is the outline of the Fairbanks Mining District (Fig.  2 ). TSZ, Teslin Suture Zone.
Image
Map of western Canada showing the location of the Lithoprobe SNORCLE lines ...
Published: 16 September 2005
Fig. 1. Map of western Canada showing the location of the Lithoprobe SNORCLE lines and the Yellowknife River, Tintina, and Teslin fault zones. Terrane nomenclature from east to west: GB, Great Bear magmatic arc; H, Hottah terrane; FS, Fort Simpson magmatic arc; N, Nahanni; CA, Cassiar; YT, Yukon
Image
Tectonic and paleogeographic restoration of Intermontane terranes ca. 195–1...
Published: 08 February 2022
Figure 12. Tectonic and paleogeographic restoration of Intermontane terranes ca. 195–185 Ma. Map restores ~450 km of dextral displacement on the Pinchi-Thibert-Teslin fault system, matches ammonoid faunal zone boundaries of Stikinia and Quesnellia ( Smith et al., 2001 ), and restores ~100 km