2008
DOI: 10.2172/958008
|View full text |Cite
|
Sign up to set email alerts
|

Preliminary Geospatial Analysis of Arctic Ocean Hydrocarbon Resources

Abstract: SummaryIce over the Arctic Ocean is predicted to become thinner and to cover less area with time (NASA, 2005). The combination of more ice-free waters for exploration and navigation, along with increasing demand for hydrocarbons and improvements in technologies for the discovery and exploitation of new hydrocarbon resources have focused attention on the hydrocarbon potential of the Arctic Basin and its margins. The purpose of this document is to 1) summarize results of a review of published hydrocarbon resourc… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2

Citation Types

0
2
0

Year Published

2011
2011
2013
2013

Publication Types

Select...
5
1

Relationship

0
6

Authors

Journals

citations
Cited by 8 publications
(2 citation statements)
references
References 20 publications
0
2
0
Order By: Relevance
“…A Polar projection of this data was shown in Long, et al (2008) at a 2 minute by 2 minute (interpolated) scale. Long, et al (2008) also show a map of predicted GHSZ thicknesses for the Arctic continental shelves. Long, et al (2008) also show a map of predicted GHSZ thicknesses for the Arctic continental shelves.…”
Section: We Have the Basic Tools For Ngh Explorationmentioning
confidence: 99%
See 1 more Smart Citation
“…A Polar projection of this data was shown in Long, et al (2008) at a 2 minute by 2 minute (interpolated) scale. Long, et al (2008) also show a map of predicted GHSZ thicknesses for the Arctic continental shelves. Long, et al (2008) also show a map of predicted GHSZ thicknesses for the Arctic continental shelves.…”
Section: We Have the Basic Tools For Ngh Explorationmentioning
confidence: 99%
“…The GHSZ thicknesses shown in the troughs by Long, et al (2008) Wood and Jung"s (2008) data added an extra dimension and a new gas play to that envisaged by Max and Lowrie (1993), who did not have access to data of sediment deposited in the troughs in the glaciated continental shelves, but rather focused on the continental margins and deeper water marine sediments. Because of the extreme cold of the Arctic Ocean bottom waters, which are usually below zero year round, GHSZ reaches 150 m thickness over very large areas and up to 300 m over considerable areas, particularly in the Amundsen Trough on the Canadian margin and the St. Anna Trough on the Barents Sea margin (Long, et al, 2008, Figs.…”
Section: We Have the Basic Tools For Ngh Explorationmentioning
confidence: 99%