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Cantwell Basin

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Journal Article
Published: 01 May 1997
Journal of Sedimentary Research (1997) 67 (3): 469–485.
...Jeffrey M. Trop; Kenneth D. Ridgway Abstract The lower Cantwell Formation, in the Cantwell basin, provides an excellent opportunity to study the petrofacies and provenance of siliciclastic deposits from an ancient thrust-top basin. The Late Cretaceous Cantwell basin formed on a series of thrust...
Journal Article
Journal: GSA Bulletin
Published: 01 May 1997
GSA Bulletin (1997) 109 (5): 505–523.
...Kenneth D. Ridgway; Jeffrey M. Trop; Arthur R. Sweet Abstract The Cantwell Formation consists of a lower sedimentary sequence as much as 4000 m thick and an upper volcanic sequence with a maximum thickness of 3750 m that was deposited in the Cantwell basin, south-central Alaska. Previous...
Journal Article
Journal: GSA Bulletin
Published: 01 December 2002
GSA Bulletin (2002) 114 (12): 1480–1504.
... part of the suture zone was development of a thrust-top basin, the Cantwell basin, in the northern part of the suture zone. Geologic mapping and compositional data suggest that the 4 km of Upper Cretaceous nonmarine and marginal marine sedimentary strata in this basin record regional subaerial uplift...
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Image
Regional map with study area and modern river sample locations annotated. U...
Published: 15 April 2019
Figure 1. Regional map with study area and modern river sample locations annotated. Upper-right inset map shows satellite image location of Figure 1 . We sampled the uplifted Tanana Basin at the Suntrana type section located near Healy, Alaska. Double Mountain (DM) is the location of Cantwell
Image
Figure 2. Geologic map and shaded relief topographic map of the Alaska Rang...
Published: 01 December 2002
of the Cantwell basin; Tug, Tng, and Qa (north of Hines Creek fault)—upper Eocene–Holocene deposits of the Tanana basin. Black arrows represent paleo–flow direction based on clast imbrication and/or trough or planar cross-stratification. Solid black arrows represent paleo–flow directions in the Cantwell Formation
Image
Paleogeographic maps and cross sections showing the inferred tectono-therma...
Published: 16 July 2019
driven exhumation and topographic development, and approach of near-trench plutons along inferred Border Ranges fault transform boundary. Abbreviations: BRF—Border Ranges fault; CB—Cantwell Basin; CMF—Castle Mountain fault; DF—Denali fault; TM—Talkeetna Mountains; WAR—western Alaska Range. (C) Late
Image
Paleogeographic maps and cross sections showing the inferred tectono-therma...
Published: 16 July 2019
driven exhumation and topographic development, and approach of near-trench plutons along inferred Border Ranges fault transform boundary. Abbreviations: BRF—Border Ranges fault; CB—Cantwell Basin; CMF—Castle Mountain fault; DF—Denali fault; TM—Talkeetna Mountains; WAR—western Alaska Range. (C) Late
Image
Paleocene–Eocene slab-window model revised from  Figure 2  to show interpre...
Published: 16 July 2019
Figure 19. Paleocene–Eocene slab-window model revised from Figure 2 to show interpretations made in this study of a trench-parallel slab-window event. Abbreviations: Cook Inlet Basin—CIB; Susitna Basin—SB; Matanuska Basin—MB; Cantwell Basin—CB; Western Alaska Range volcanics—WV; Jack River
Image
Figure 1. (A) Map showing the present distribution of accreted terranes, up...
Published: 01 January 2008
the Cantwell basin (CB), Pass Creek area (PC), and Wrangell Mountains basin (WB). Uppermost Cretaceous and younger strata and magmatic belts formed within a juvenile continental margin composed of the allochthonous Wrangellia composite terrane (WCT) and para-autochthonous Paleozoic–Mesozoic metamorphic rocks
Image
Generalized geologic map of south-central Alaska shows the distribution of ...
Published: 10 June 2021
. Locations of new U-Pb detrital zircon samples reported in this study are denoted by the yellow dots. Locations of previously published U-Pb detrital zircon samples are shown in blue. See text for references. Abbreviations: AAP—Aleutian-Alaska Peninsula volcanic arc; CB—Cantwell basin; CIB—Cook Inlet basin
Image
(A) Previously proposed Paleocene–Eocene slab window summary figure, based ...
Published: 16 July 2019
Basin—SB; Matanuska Basin—MB; Tanana Basin—TB; Cantwell Basin—CB; Western Alaska Range volcanics—WV; Jack River volcanics—JV; Central Talkeetna volcanics—CTV; Caribou Hill volcanics—CV; Tanana Valley volcanics—TV; Sifton volcanics—SV; Denali fault—DF; Border Ranges fault system—BRF; Castle Mountain
Journal Article
Journal: Geosphere
Published: 26 June 2019
Geosphere (2019) 15 (4): 1066–1101.
... ( Csejtey et al., 1992 ; Ridgway et al., 2002 ). Coeval with metamorphism of Kahiltna basin strata in the southern part of the suture zone was development of a thrust-top basin, the Cantwell basin, which is presently exposed between the Hines Creek and Denali fault systems. Compositional, detrital...
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Figure 1. (A) Index map showing location of study area in south-central Ala...
Published: 01 December 2002
Wrangellia composite terrane and Upper Jurassic–Upper Cretaceous deposits of the Kahiltna basin (labeled KJk). Upper Cretaceous–lower Eocene deposits of the Cantwell basin are labeled Kcs and Tcv on (Caption continued on p. 1483.)
Journal Article
Journal: Geosphere
Published: 15 April 2019
Geosphere (2019) 15 (3): 682–701.
...Figure 1. Regional map with study area and modern river sample locations annotated. Upper-right inset map shows satellite image location of Figure 1 . We sampled the uplifted Tanana Basin at the Suntrana type section located near Healy, Alaska. Double Mountain (DM) is the location of Cantwell...
FIGURES | View All (13)
Journal Article
Journal: PALAIOS
Published: 01 October 2016
PALAIOS (2016) 31 (10): 479–482.
.... The geologic age of the upper Cantwell Formation is Paleocene to Eocene with dates of 60–55.5 Ma ( Cole et al. 1999 ). Gilbert et al. (1976) named this upper unit the Teklanika Formation, but the unit name was not accepted by subsequent workers. In the most recent basin-wide study of the stratigraphy...
FIGURES
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Figure 6. Representative measured stratigraphic sections from strata of the...
Published: 01 December 2002
Figure 6. Representative measured stratigraphic sections from strata of the Cantwell and Tanana sedimentary basins. Data were collected as bed-bed measurements by using a Jacob's staff. For detailed measured sections of the upper Cantwell Formation, see Cole et al. (1999) . The Usibelli Group
Journal Article
Journal: PALAIOS
Published: 01 July 2009
PALAIOS (2009) 24 (7): 466–472.
... a basin formed between Wrangellia and the margin of North America during the accretion of the former ( Ridgway et al., 1997 ). Rocks of the Lower Cantwell Formation are comprised of conglomerates, organic-rich and fossiliferous sandstones, mudstones, and coals. The fluvial setting has been interpreted...
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Journal Article
Journal: Geology
Published: 01 August 2014
Geology (2014) 42 (8): 719–722.
.... 295 , p. 979 – 980 , doi:10.1126/science.1068920 . Ricklefs R.E. Miller G.L. , 2000 , Ecology ( fourth edition ): New York, W.H . Freeman and Company , 822 p. Ridgway K.D. Trop J.M. Sweet A.R. , 1997 , Thrust-top basin formation along a suture zone, Cantwell...
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Journal Article
Journal: PALAIOS
Published: 01 June 2012
PALAIOS (2012) 27 (6): 395–400.
... is Paleocene to Eocene in age with dates of ranging from 60 to 55.5 Ma ( Cole et al., 1999 ). Gilbert et al. (1976) named the upper unit the Teklanika Formation, but subsequent workers have not accepted this designation. In the most recent basin-wide study of the stratigraphy of the Cantwell Formation...
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Journal Article
Published: 22 April 2004
Canadian Journal of Earth Sciences (2004) 41 (4): 457–480.
.... Sedimentary deposits of the Colorado Creek basin (TKs in Fig.  2 ) are restricted exclusively to the south side of the McKinley fault and were previously correlated with the lower Cantwell Formation, which is restricted to the north side of the McKinley fault (Kcs in Fig.  2 ; Csejtey et al. 1984 , 1992...
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