Stratigraphic sequence of the Gile Mountain and Waits River Formations near Royalton, Vermont
1980; Geological Society of America; Volume: 91; Issue: 5 Linguagem: Inglês
10.1130/0016-7606(1980)91 2.0.co;2
ISSN1943-2674
AutoresGeorge W. Fisher, Paul Karabinos,
Tópico(s)Geological and Geochemical Analysis
ResumoResearch Article| May 01, 1980 Stratigraphic sequence of the Gile Mountain and Waits River Formations near Royalton, Vermont GEORGE W. FISHER; GEORGE W. FISHER 1Department of Earth and Planetary Sciences, Johns Hopkins University, Baltimore, Maryland 21218 Search for other works by this author on: GSW Google Scholar PAUL KARABINOS PAUL KARABINOS 1Department of Earth and Planetary Sciences, Johns Hopkins University, Baltimore, Maryland 21218 Search for other works by this author on: GSW Google Scholar GSA Bulletin (1980) 91 (5): 282–286. https://doi.org/10.1130/0016-7606(1980)91 2.0.CO;2 Article history first online: 01 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation GEORGE W. FISHER, PAUL KARABINOS; Stratigraphic sequence of the Gile Mountain and Waits River Formations near Royalton, Vermont. GSA Bulletin 1980;; 91 (5): 282–286. doi: https://doi.org/10.1130/0016-7606(1980)91 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 stratigraphic sequence of the Gile Mountain and Waits River Formations, two major Silurian-Devonian lithostratigraphic units in eastern Vermont, has long been controversial. This uncertainty has given rise to numerous difficulties in interpreting the regional structure of eastern Vermont. Extensive sequences of compositionally graded beds at 19 localities across the Gile Mountain belt near Royalton, Vermont, show that the Gile Mountain Formation is younger than the Waits River Formation, indicating that the belt is a syncline. 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.
Referência(s)