FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2314207397> ?p ?o ?g. }

• W2314207397 endingPage "196" @default.
• W2314207397 startingPage "183" @default.
• W2314207397 abstract "Research Article| January 01, 2011 Petrogenesis of the McDermott Formation trachyandesite, San Juan basin, Colorado and New Mexico Daniel Wegert; Daniel Wegert ∗ 1Department of Geology, Baylor University, One Bear Place #97354, Waco, Texas 76798, U.S.A. ∗Correspondence should be addressed to: dwegert@mclennan.edu Search for other works by this author on: GSW Google Scholar Don F. Parker Don F. Parker 2Department of Geology, Baylor University, One Bear Place #97354, Waco, Texas 76798, U.S.A. Search for other works by this author on: GSW Google Scholar Rocky Mountain Geology (2011) 46 (2): 183–196. https://doi.org/10.2113/gsrocky.46.2.183 Article history received: 19 May 2009 rev-recd: 08 Apr 2011 accepted: 28 Jul 2011 first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation Daniel Wegert, Don F. Parker; Petrogenesis of the McDermott Formation trachyandesite, San Juan basin, Colorado and New Mexico. Rocky Mountain Geology 2011;; 46 (2): 183–196. doi: https://doi.org/10.2113/gsrocky.46.2.183 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search nav search search input Search input auto suggest search filter All ContentBy SocietyRocky Mountain Geology Search Advanced Search Abstract Lahar deposits within the Late Cretaceous McDermott Formation (Maastrichtian) contain abundant trachyandesite volcanic clasts with a narrow range of whole rock compositions. The outcrop pattern and thickness variations of the McDermott Formation suggest a source located in the general area of the present-day La Plata Mountains. Major and trace element trends indicate a possible petrogenetic relationship between the McDermott trachyandesite and La Plata Mountains intrusive rocks. Incompatible trace element compositions show subduction signatures in the trachyandesite and La Plata intrusive rocks, as well as in lower crustal xenoliths from the nearby Navajo volcanic field. Trace element patterns of Proterozoic units from the adjacent San Juan uplift rule out involvement of these upper crustal units in McDermott petrogenesis. Near zero ∊Ndt (−1.94 and 0.47) values rule out a Precambrian crustal source for these magmas as crustal values typically range from −6 to −18. Ba/La vs. Nb/La plots and ∊Ndt data suggest a subduction-modified continental lithospheric mantle source for these rocks. This lithospheric mantle may have acquired its orogenic trace-element signature during formation of the Proterozoic Yavapai terrane, which underlies the region. You do not currently have access to this article." @default.
• W2314207397 created "2016-06-24" @default.
• W2314207397 creator A5044790276 @default.
• W2314207397 creator A5089498529 @default.
• W2314207397 date "2011-09-01" @default.
• W2314207397 modified "2023-09-26" @default.
• W2314207397 title "Petrogenesis of the McDermott Formation trachyandesite, San Juan basin, Colorado and New Mexico" @default.
• W2314207397 cites W1972635099 @default.
• W2314207397 cites W1997417867 @default.
• W2314207397 cites W2000521957 @default.
• W2314207397 cites W2015580967 @default.
• W2314207397 cites W2016195231 @default.
• W2314207397 cites W2018717489 @default.
• W2314207397 cites W2019875441 @default.
• W2314207397 cites W2086263915 @default.
• W2314207397 cites W2087511024 @default.
• W2314207397 cites W2087734990 @default.
• W2314207397 cites W2091835213 @default.
• W2314207397 cites W2104609449 @default.
• W2314207397 cites W2108641227 @default.
• W2314207397 cites W2126242954 @default.
• W2314207397 cites W2127172635 @default.
• W2314207397 cites W2157099954 @default.
• W2314207397 cites W2159956318 @default.
• W2314207397 cites W2317139889 @default.
• W2314207397 cites W2337175154 @default.
• W2314207397 cites W2505916859 @default.
• W2314207397 doi "https://doi.org/10.2113/gsrocky.46.2.183" @default.
• W2314207397 hasPublicationYear "2011" @default.
• W2314207397 type Work @default.
• W2314207397 sameAs 2314207397 @default.
• W2314207397 citedByCount "7" @default.
• W2314207397 countsByYear W23142073972014 @default.
• W2314207397 countsByYear W23142073972018 @default.
• W2314207397 countsByYear W23142073972019 @default.
• W2314207397 countsByYear W23142073972021 @default.
• W2314207397 countsByYear W23142073972022 @default.
• W2314207397 countsByYear W23142073972023 @default.
• W2314207397 crossrefType "journal-article" @default.
• W2314207397 hasAuthorship W2314207397A5044790276 @default.
• W2314207397 hasAuthorship W2314207397A5089498529 @default.
• W2314207397 hasConcept C12294951 @default.
• W2314207397 hasConcept C127313418 @default.
• W2314207397 hasConcept C151730666 @default.
• W2314207397 hasConcept C161191863 @default.
• W2314207397 hasConcept C161509811 @default.
• W2314207397 hasConcept C166957645 @default.
• W2314207397 hasConcept C169212394 @default.
• W2314207397 hasConcept C17409809 @default.
• W2314207397 hasConcept C205649164 @default.
• W2314207397 hasConcept C2778805511 @default.
• W2314207397 hasConcept C41008148 @default.
• W2314207397 hasConcept C44938399 @default.
• W2314207397 hasConceptScore W2314207397C12294951 @default.
• W2314207397 hasConceptScore W2314207397C127313418 @default.
• W2314207397 hasConceptScore W2314207397C151730666 @default.
• W2314207397 hasConceptScore W2314207397C161191863 @default.
• W2314207397 hasConceptScore W2314207397C161509811 @default.
• W2314207397 hasConceptScore W2314207397C166957645 @default.
• W2314207397 hasConceptScore W2314207397C169212394 @default.
• W2314207397 hasConceptScore W2314207397C17409809 @default.
• W2314207397 hasConceptScore W2314207397C205649164 @default.
• W2314207397 hasConceptScore W2314207397C2778805511 @default.
• W2314207397 hasConceptScore W2314207397C41008148 @default.
• W2314207397 hasConceptScore W2314207397C44938399 @default.
• W2314207397 hasIssue "2" @default.
• W2314207397 hasLocation W23142073971 @default.
• W2314207397 hasOpenAccess W2314207397 @default.
• W2314207397 hasPrimaryLocation W23142073971 @default.
• W2314207397 hasRelatedWork W1964524950 @default.
• W2314207397 hasRelatedWork W2085480428 @default.
• W2314207397 hasRelatedWork W2103355267 @default.
• W2314207397 hasRelatedWork W2122544454 @default.
• W2314207397 hasRelatedWork W2736004005 @default.
• W2314207397 hasRelatedWork W2798082128 @default.
• W2314207397 hasRelatedWork W2919497212 @default.
• W2314207397 hasRelatedWork W2975723042 @default.
• W2314207397 hasRelatedWork W3008982824 @default.
• W2314207397 hasRelatedWork W4234926551 @default.
• W2314207397 hasVolume "46" @default.
• W2314207397 isParatext "false" @default.
• W2314207397 isRetracted "false" @default.
• W2314207397 magId "2314207397" @default.
• W2314207397 workType "article" @default.