1962
DOI: 10.4095/100554
|View full text |Cite
|
Sign up to set email alerts
|

Banks, Victoria, and Stefansson islands, Arctic Archipelago

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

0
54
0

Year Published

1981
1981
2016
2016

Publication Types

Select...
5
3
1

Relationship

0
9

Authors

Journals

citations
Cited by 57 publications
(54 citation statements)
references
References 0 publications
0
54
0
Order By: Relevance
“…In fact, they are from the Kanguk Formation (Felix & Burbridge 1976, Manum 1991. Marine microplankton from nearby Banks Island documented by Thorsteinsson & Tozer (1962) are also similar to the assemblages from Ellef Rignes and Graham islands. This major work was completed by correspondence between Melbourne and Oslo.…”
Section: Alcheringamentioning
confidence: 74%
“…In fact, they are from the Kanguk Formation (Felix & Burbridge 1976, Manum 1991. Marine microplankton from nearby Banks Island documented by Thorsteinsson & Tozer (1962) are also similar to the assemblages from Ellef Rignes and Graham islands. This major work was completed by correspondence between Melbourne and Oslo.…”
Section: Alcheringamentioning
confidence: 74%
“…2). Sedimentary strata of the Shaler Supergroup, a 4-km thick succession of carbonate and evaporitic rocks (Young, 1981;Rainbird et al, 1994Rainbird et al, , 2014 are intruded by Thorsteinsson and Tozer, 1962). Location of study sites Gossan Hill (GH) and Sill Gossan (SG) shown as yellow triangles on map.…”
Section: Study Areamentioning
confidence: 99%
“…The northeast plateau consists of Devonian age limestone and the southern uplands consist of Precambrian gabbro rocks. These rocks form upland terrain rising to elevations of ~700 m. By contrast, the majority of the central and western lowlands are underlain by poorly consolidated Mesozoic-age sediments that vary in lithology from shale of the Christopher Formation to sands and gravels of the Eureka Sound and Beaufort Formations (Thorsteinsson and Tozer, 1962;Miall, 1979;Fyles, 1994). Fluvial dissection has resulted in relative relief that varies from less than 50 m to over 250 m. The interfluves and upper slopes are covered with an extensive but thin veneer of till and glacio-fluvial deposits.…”
Section: Structure and Reliefmentioning
confidence: 99%
“…These water bodies are ice-covered for more than 8-9 months of the year. Tozer and Thorsteinsson, 1962;Thorsteinsson and Tozer, 1964 …”
Section: Introductionmentioning
confidence: 99%