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Title: Arctic Work.


Abstract not provided.

Publication Date:
Research Org.:
Sandia National Lab. (SNL-NM), Albuquerque, NM (United States)
Sponsoring Org.:
USDOE Office of Science (SC), Biological and Environmental Research (BER) (SC-23)
OSTI Identifier:
Report Number(s):
DOE Contract Number:
Resource Type:
Resource Relation:
Conference: Proposed for presentation at the University of Alaska Fairbanks Visit held May 11, 2016 in Albuquerque, NM.
Country of Publication:
United States

Citation Formats

Halloran, Amy Randolph, and Ivey, Mark D. Arctic Work.. United States: N. p., 2016. Web.
Halloran, Amy Randolph, & Ivey, Mark D. Arctic Work.. United States.
Halloran, Amy Randolph, and Ivey, Mark D. 2016. "Arctic Work.". United States. doi:.
title = {Arctic Work.},
author = {Halloran, Amy Randolph and Ivey, Mark D.},
abstractNote = {Abstract not provided.},
doi = {},
journal = {},
number = ,
volume = ,
place = {United States},
year = 2016,
month = 5

Other availability
Please see Document Availability for additional information on obtaining the full-text document. Library patrons may search WorldCat to identify libraries that hold this conference proceeding.

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  • This workshop was held May 2--7, 1993 in Anchorage, Alaska. The purpose of this conference was to provide a multidisciplinary forum for exchange of state-of-the-art information on air, water, and land pollution in the Arctic. The workshop addressed Arctic pollution in its broadest sense, dealing with pollution from trace metals, organic compounds, and contamination from radionuclides. Fifty papers are presented in these proceedings.
  • The Arctic Creek section is dissimilar to the typical Cretaceous section exposed elsewhere in Ignek Valley. The more typical Ignek Valley sequence consists of Kingak Shale (Jurassic to Neocomian), Kemik Sandstone (Hauterivian), Pebble Shale (Hauterivian-Barremian), Hue Shale ( Santonian), and turbidites of the Canning Formation (Campanian to Paleocene). The two main differences that distinguish the Arctic Creek section from the typical Ignek Valley section are: (1) lack of the regionally persistent Kemik Sandstone in the Arctic Creek section, and (2) lack of Albian turbidites in the typical Ignek Valley section. The Arctic Creek section is more similar to the Cretaceousmore » section exposed at Bathtub Ridge about 180 km to the southeast. The Bathtub Ridge section consists of black shale with local siltstone beds (Jurassic to Lower Cretaceous), manganiferous shale, interbedded shale and siltstone turbidites (Albian), and sandstone turbidites (Albian.). The authors believe that the Arctic Creek and Bathtub Ridge sections were once part of a continuous depositional basin, and that the Arctic Creek section has been thrust northward into juxtaposition with the typical Ignek Valley strata.« less
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  • Volume 4 contains papers on the following topics: arctic/polar technology and development; ice properties; ice engineering; applied ice mechanics; ice-structure interaction; arctic structures and operations; frozen soil properties; and Russian Arctic development. In addition to the regular topics covered in OMAE conferences, there has been a special workshop as part of this year`s conference. In keeping with issues of current interest, there is a workshop on development of oil resources in the Russian Arctic. Over two days, papers dealing with development of oil and gas resources in the Russian Arctic are presented. Volume 4 contains papers from this workshop. Somemore » of the papers have been processed separately for inclusion on the data base.« less