FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2110087776> ?p ?o ?g. }

• W2110087776 endingPage "72" @default.
• W2110087776 startingPage "72" @default.
• W2110087776 abstract "Research Article| January 01, 1989 Pedogenic slickensides, indicators of strain and deformation processes in redbed sequences of the Appalachian foreland Mary Beth Gray; Mary Beth Gray 1Department of Geological Sciences, University of Rochester, Rochester, New York 14627 Search for other works by this author on: GSW Google Scholar Richard P. Nickelsen Richard P. Nickelsen 2Department of Geology, Bucknell University, Lewisburg, Pennsylvania 17837 Search for other works by this author on: GSW Google Scholar Author and Article Information Mary Beth Gray 1Department of Geological Sciences, University of Rochester, Rochester, New York 14627 Richard P. Nickelsen 2Department of Geology, Bucknell University, Lewisburg, Pennsylvania 17837 Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1989) 17 (1): 72–75. https://doi.org/10.1130/0091-7613(1989)017<0072:PSIOSA>2.3.CO;2 Article history First Online: 02 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 Mary Beth Gray, Richard P. Nickelsen; Pedogenic slickensides, indicators of strain and deformation processes in redbed sequences of the Appalachian foreland. Geology 1989;; 17 (1): 72–75. doi: https://doi.org/10.1130/0091-7613(1989)017<0072:PSIOSA>2.3.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 SocietyGeology Search Advanced Search Abstract Pedogenic slickensides are convex-concave slip surfaces that form during expansion/contraction in expansive clay soils such as Vertisols. In the central Appalachians, they occur near the tops of fining-upward cycles in Paleozoic redbeds such as the Bloomsburg, Catskill, and Mauch Chunk Formations. Pedogenic slickensides are found in association with other pedogenic (or paleosol) features such as clay-skinned peds, in situ calcareous nodules, and root impressions. Repeated movements along these shear planes during pedogenesis produce strongly aligned clay particles adjacent to pedogenic slickensides; as a result, they are preserved as discrete fractures throughout diagenesis, compaction, and superimposed tectonic deformation. During whole-rock deformation, pedogenic slickensides segregate penetratively deformed rocks into independent, foliated packets and serve as discontinuities that are followed by later structural features. Because the original morphology of pedogenic slickensides is known, they can be used as crude strain markers. 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." @default.
• W2110087776 created "2016-06-24" @default.
• W2110087776 creator A5033046710 @default.
• W2110087776 creator A5081204627 @default.
• W2110087776 date "1989-01-01" @default.
• W2110087776 modified "2023-09-26" @default.
• W2110087776 title "Pedogenic slickensides, indicators of strain and deformation processes in redbed sequences of the Appalachian foreland" @default.
• W2110087776 cites W1951836618 @default.
• W2110087776 cites W1990226939 @default.
• W2110087776 cites W1995207169 @default.
• W2110087776 cites W2022895034 @default.
• W2110087776 cites W2028141898 @default.
• W2110087776 cites W2031848534 @default.
• W2110087776 cites W2037287448 @default.
• W2110087776 cites W2081959850 @default.
• W2110087776 cites W2082167506 @default.
• W2110087776 cites W2082205876 @default.
• W2110087776 cites W2108395542 @default.
• W2110087776 cites W2222103683 @default.
• W2110087776 cites W261129832 @default.
• W2110087776 cites W2094662357 @default.
• W2110087776 cites W340143994 @default.
• W2110087776 doi "https://doi.org/10.1130/0091-7613(1989)017<0072:psiosa>2.3.co;2" @default.
• W2110087776 hasPublicationYear "1989" @default.
• W2110087776 type Work @default.
• W2110087776 sameAs 2110087776 @default.
• W2110087776 citedByCount "47" @default.
• W2110087776 countsByYear W21100877762013 @default.
• W2110087776 countsByYear W21100877762014 @default.
• W2110087776 countsByYear W21100877762015 @default.
• W2110087776 countsByYear W21100877762016 @default.
• W2110087776 countsByYear W21100877762018 @default.
• W2110087776 countsByYear W21100877762019 @default.
• W2110087776 countsByYear W21100877762020 @default.
• W2110087776 countsByYear W21100877762022 @default.
• W2110087776 crossrefType "journal-article" @default.
• W2110087776 hasAuthorship W2110087776A5033046710 @default.
• W2110087776 hasAuthorship W2110087776A5081204627 @default.
• W2110087776 hasConcept C127313418 @default.
• W2110087776 hasConcept C151730666 @default.
• W2110087776 hasConcept C161191863 @default.
• W2110087776 hasConcept C193748577 @default.
• W2110087776 hasConcept C199360897 @default.
• W2110087776 hasConcept C2778447006 @default.
• W2110087776 hasConcept C2778805511 @default.
• W2110087776 hasConcept C41008148 @default.
• W2110087776 hasConcept C77928131 @default.
• W2110087776 hasConceptScore W2110087776C127313418 @default.
• W2110087776 hasConceptScore W2110087776C151730666 @default.
• W2110087776 hasConceptScore W2110087776C161191863 @default.
• W2110087776 hasConceptScore W2110087776C193748577 @default.
• W2110087776 hasConceptScore W2110087776C199360897 @default.
• W2110087776 hasConceptScore W2110087776C2778447006 @default.
• W2110087776 hasConceptScore W2110087776C2778805511 @default.
• W2110087776 hasConceptScore W2110087776C41008148 @default.
• W2110087776 hasConceptScore W2110087776C77928131 @default.
• W2110087776 hasIssue "1" @default.
• W2110087776 hasLocation W21100877761 @default.
• W2110087776 hasOpenAccess W2110087776 @default.
• W2110087776 hasPrimaryLocation W21100877761 @default.
• W2110087776 hasRelatedWork W1999667573 @default.
• W2110087776 hasRelatedWork W2027688938 @default.
• W2110087776 hasRelatedWork W2118995100 @default.
• W2110087776 hasRelatedWork W2124399314 @default.
• W2110087776 hasRelatedWork W2147654633 @default.
• W2110087776 hasRelatedWork W2152165443 @default.
• W2110087776 hasRelatedWork W2340485914 @default.
• W2110087776 hasRelatedWork W2368747801 @default.
• W2110087776 hasRelatedWork W3130151701 @default.
• W2110087776 hasRelatedWork W4289755559 @default.
• W2110087776 hasVolume "17" @default.
• W2110087776 isParatext "false" @default.
• W2110087776 isRetracted "false" @default.
• W2110087776 magId "2110087776" @default.
• W2110087776 workType "article" @default.