FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4233640557> ?p ?o ?g. }

• W4233640557 endingPage "1387" @default.
• W4233640557 startingPage "1387" @default.
• W4233640557 abstract "Research Article| November 01, 2007 Throughgoing fractures in layered carbonate rocks Michael R. Gross; Michael R. Gross 1Department of Earth Sciences, Florida International University, Miami, Florida 33199, USA Search for other works by this author on: GSW Google Scholar Yehuda Eyal Yehuda Eyal 2Department of Geological and Environmental Sciences, Ben-Gurion University of the Negev, Beer Sheva 84105, Israel Search for other works by this author on: GSW Google Scholar GSA Bulletin (2007) 119 (11-12): 1387–1404. https://doi.org/10.1130/0016-7606(2007)119[1387:TFILCR]2.0.CO;2 Article history received: 31 May 2006 rev-recd: 16 May 2007 accepted: 28 May 2007 first online: 08 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation Michael R. Gross, Yehuda Eyal; Throughgoing fractures in layered carbonate rocks. GSA Bulletin 2007;; 119 (11-12): 1387–1404. doi: https://doi.org/10.1130/0016-7606(2007)119[1387:TFILCR]2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu nav search search input Search input auto suggest search filter All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract Fracture surveys were conducted across a broad anticline in southern Israel in order to investigate the development and geometries of throughgoing fractures in layered carbonate rocks. At Halukim anticline, throughgoing fractures form by the linkage and coalescence of preexisting, bed-confined joints. Thus the internal morphology of these structures is highly segmented, often consisting of vertically aligned zones of subparallel fractures and bed partings linked together across the stratigraphy. The large population (n = 132) of throughgoing fractures represents a continuum of structures at various stages of development that can be classified into three main geometric categories corresponding to increasing levels of brittle strain: incipient, linked, and linked with aperture. Despite the wide variety of internal morphologies and geometries, the throughgoing fractures display a consistent east-northeast–west-southwest orientation, parallel to a set of bed- confined cross joints. The spatial distribution of throughgoing fractures varies as a function of structural position, the highest frequency and estimated strain intensity being located at the fold crest. Results suggest that throughgoing fractures develop only after a critical level of strain is achieved, as quantified by the density of bed-confined joints. Throughgoing fractures are multilayer structures that may greatly enhance the connectivity of a fracture network; therefore, understanding their formation, geometry, and distribution may contribute to efforts of flow modeling in fractured carbonate rocks. You do not currently have access to this article." @default.
• W4233640557 created "2022-05-12" @default.
• W4233640557 creator A5084540630 @default.
• W4233640557 creator A5087584536 @default.
• W4233640557 date "2007-01-01" @default.
• W4233640557 modified "2023-10-18" @default.
• W4233640557 title "Throughgoing fractures in layered carbonate rocks" @default.
• W4233640557 doi "https://doi.org/10.1130/b26049" @default.
• W4233640557 hasPublicationYear "2007" @default.
• W4233640557 type Work @default.
• W4233640557 citedByCount "1" @default.
• W4233640557 countsByYear W42336405572018 @default.
• W4233640557 crossrefType "journal-article" @default.
• W4233640557 hasAuthorship W4233640557A5084540630 @default.
• W4233640557 hasAuthorship W4233640557A5087584536 @default.
• W4233640557 hasConcept C116637073 @default.
• W4233640557 hasConcept C127313418 @default.
• W4233640557 hasConcept C151730666 @default.
• W4233640557 hasConcept C161191863 @default.
• W4233640557 hasConcept C23123220 @default.
• W4233640557 hasConcept C2778805511 @default.
• W4233640557 hasConcept C41008148 @default.
• W4233640557 hasConcept C77928131 @default.
• W4233640557 hasConceptScore W4233640557C116637073 @default.
• W4233640557 hasConceptScore W4233640557C127313418 @default.
• W4233640557 hasConceptScore W4233640557C151730666 @default.
• W4233640557 hasConceptScore W4233640557C161191863 @default.
• W4233640557 hasConceptScore W4233640557C23123220 @default.
• W4233640557 hasConceptScore W4233640557C2778805511 @default.
• W4233640557 hasConceptScore W4233640557C41008148 @default.
• W4233640557 hasConceptScore W4233640557C77928131 @default.
• W4233640557 hasIssue "11" @default.
• W4233640557 hasLocation W42336405571 @default.
• W4233640557 hasOpenAccess W4233640557 @default.
• W4233640557 hasPrimaryLocation W42336405571 @default.
• W4233640557 hasRelatedWork W1606027898 @default.
• W4233640557 hasRelatedWork W1972822417 @default.
• W4233640557 hasRelatedWork W2085252764 @default.
• W4233640557 hasRelatedWork W2099228511 @default.
• W4233640557 hasRelatedWork W2099947365 @default.
• W4233640557 hasRelatedWork W2113842777 @default.
• W4233640557 hasRelatedWork W2152273076 @default.
• W4233640557 hasRelatedWork W2283185939 @default.
• W4233640557 hasRelatedWork W2340943978 @default.
• W4233640557 hasRelatedWork W2979898295 @default.
• W4233640557 hasVolume "119" @default.
• W4233640557 isParatext "false" @default.
• W4233640557 isRetracted "false" @default.
• W4233640557 workType "article" @default.