The DOI matches its Crossref record.
Late Quaternary geology and geochronology of the central continental shelf of western Canada
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At its maximum extent, the Cordilleran Ice Sheet flowed from the Coast Mountain Range westward across the present coastal islands and toward the continental shelf margin.
“At its maximum extent, the Cordilleran Ice Sheet flowed from the Coast Mountain Range westward across the present coastal islands and toward the continental shelf margin (Barrie & Conway, 1999;Luternauer, Clague, et al., 1989;Luternauer, Conway, et al., 1989).”
From Retreat of the Western Cordilleran Ice Sheet Margin During the Last Deglaciation (2018) · cites this paper as Luternauer, Conway, et al., 1989
At its maximum extent, the Cordilleran Ice Sheet flowed from the Coast Mountain Range westward across the present coastal islands and toward the continental shelf margin.
“At its maximum extent, the Cordilleran Ice Sheet flowed from the Coast Mountain Range westward across the present coastal islands and toward the continental shelf margin (Barrie & Conway, 1999;Luternauer, Clague, et al., 1989;Luternauer, Conway, et al., 1989).”
From Retreat of the Western Cordilleran Ice Sheet Margin During the Last Deglaciation (2018) · cites this paper as Luternauer, Clague, et al., 1989
Citations
Cites
No references could be resolved yet.
Research works printed but not linked: 11
- Blaise, 1989, Clay-mineral assemblages from late Quaternary deposits on Vancouver Island, southwestern British Columbia, Canada, Quat. Res., 31, 41, 10.1016/0033-5894(89)90084-7 · DOI
- Blaise, 1988, Clay mineralogy of late Pleistocene glacial deposits in Chilliwack Valley, southwestern British Columbia, Geol. Surv. Can. Pap., 88-1E, 25
- Clague, 1981, Late Quaternary geology and geochronology of British Columbia. Part 2: Summary and discussion of radiocarbon-dated Quaternary history, Geol. Surv. Can. Pap., 80-35, 41
- Clague, 1985, Deglaciation of the Prince Rupert Kitimat area, British Columbia, Can. J. Earth Sci., 22, 256, 10.1139/e85-022 · DOI · Paper page
- Conway, 1984, Longest core of Quaternary sediments from Queen Charlotte Sound: Preliminary description and interpretation, Geol. Surv. Can. Pap, 84-1A, 647
- Duggan, 1986, Distribution of surficial sediment and major bedforms, Goose I. Bank, Queen Charlotte Sound, central continental shelf off British Columbia, Geol. Surv. Can. Open File Rep., 1329
- Holtzapffel, 1985, Les minéraux argileux: préparation, analyse diffractometrique et détermination, Soc. Geol. Nord Mem., 12, 136
- Luternauer, 1983, Late Quaternary morphologic development and sedimentation, central British Columbia continental shelf, Geol. Surv. Can. Pap., 83-21, 38
- Luternauer, 1989, Late Pleistocene terrestrial deposits on the continental shelf of western Canada: Evidence for rapid sea-level change at the end of the last glaciation, Geology, 17, 357, 10.1130/0091-7613(1989)017<0357:LPTDOT>2.3.CO;2 · DOI
- Prest, 1984, Late Wisconsinan glacier complex, Geol. Surv. Can.
- Shouldice, 1971, Geology of the western Canadian continental shelf, Bull. Can. Pet. Geol., 19, 405
Cited by
Sorted by citations
Retreat of the Western Cordilleran Ice Sheet Margin During the Last Deglaciation
Darvill, C. M., Menounos, B., Goehring, B. M., Lian, O. B., & Caffee, M. W. (2018) · Geophysical Research Letters · doi:10.1029/2018gl079419 · Cited by 105
Metadata
- Authors
- Luternauer, J. L., Conway, K. W., Clague, J. J., & Blaise, B.
- Venue
- Marine Geology
- Publisher
- Elsevier BV
- Published
- 1989-09
- Volume
- 89
- Issue
- 1-2
- Pages
- 57-68
- ISSN
- 0025-3227
- Cited by
- 43
- References
- 0
- Language
- en
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