Artigo Revisado por pares

UNMETAMORPHOSED SANDSTONE IN NORTHERN LABRADOR

1964; Geological Society of America; Volume: 75; Issue: 6 Linguagem: Inglês

10.1130/0016-7606(1964)75[569

ISSN

1943-2674

Autores

Everett P. Wheeler,

Tópico(s)

Hydrocarbon exploration and reservoir analysis

Resumo

Research Article| June 01, 1964 UNMETAMORPHOSED SANDSTONE IN NORTHERN LABRADOR E. P WHEELER, 2ND E. P WHEELER, 2ND DEPT. GEOLOGY, CORNELL UNIVERSITY, ITHACA, N. Y. Search for other works by this author on: GSW Google Scholar Author and Article Information E. P WHEELER, 2ND DEPT. GEOLOGY, CORNELL UNIVERSITY, ITHACA, N. Y. Publisher: Geological Society of America Received: 13 Apr 1962 First Online: 02 Mar 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Copyright © 1964, The Geological Society of America, Inc. Copyright is not claimed on any material prepared by U.S. government employees within the scope of their employment. GSA Bulletin (1964) 75 (6): 569–570. https://doi.org/10.1130/0016-7606(1964)75[569:USINL]2.0.CO;2 Article history Received: 13 Apr 1962 First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation E. P WHEELER; UNMETAMORPHOSED SANDSTONE IN NORTHERN LABRADOR. GSA Bulletin 1964;; 75 (6): 569–570. doi: https://doi.org/10.1130/0016-7606(1964)75[569:USINL]2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract The Siamarnekh formation at 2000 feet elevation in northern Labrador is an unmetamorphosed, red to pale orange, unfossiliferous sand-stone that is uniformly medium grained except for a small amount of conglomerate near the base. It is a moderately mature multicycle deposit with a composition covering the subarkose range. It is cut by a major west-dipping low-angle thrust fault. Northeasterly movement of Pleistocene glaciation can account for the known distribution of indicators from this formation. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

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