FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4205127744> ?p ?o ?g. }

• W4205127744 abstract "Fractures can provide valuable information on the tectonic evolution of the Earth’s crust. Our field observation data, rock core data, and thin section observations reveal several horizontal fractures in the Cenozoic mudstone strata in the western Qaidam Basin, Qinghai Province, China. These horizontal fractures have rough surfaces and are filled by gypsum. The fractures are mainly curved; however, some straight fractures are also found. There are many intersections between adjacent curved fractures, which often adjoin to form “T” shape fractures. Fracture apertures are mainly between 1 mm and 1 cm, with a maximum of 3 cm. Both the size and density of fractures decrease as strata denudation thickness decreases and depth of burial increases. Horizontal fractures are only found in a core area of anticlines with severe strata denudation. Accordingly, these fractures are related to vertical extension due to residual stress in the process of rapid uplift and denudation. The horizontal fractures cut earlier vertical tectonic fractures, indicating their formation after tectonic extrusion. Electron spin resonance (ESR) dating of fracture-filling materials revealed that horizontal fractures appeared in two stages. The first stage was approximately 1.8 Ma ago, while the second stage was approximately 0.3 Ma ago. The size and density of the later-stage horizontal fractures are markedly greater than the earlier-stage fractures. Based on the driving stress when fractures are formed, which is obtained from fracture parameters, the denudation rate in the later stage was approximately 2∼3-fold greater than that in the earlier stage. According to the evidence, during the Quaternary, the western Qaidam Basin experienced pulsating tectonic extrusion, producing uplift and denudation and an increase in tectonic activity. Such findings suggest a gradual increase in episodic tectonic activity in the entire Tibetan Plateau region during the Quaternary." @default.
• W4205127744 created "2022-01-25" @default.
• W4205127744 creator A5017732563 @default.
• W4205127744 creator A5030452192 @default.
• W4205127744 creator A5040825987 @default.
• W4205127744 creator A5058749575 @default.
• W4205127744 creator A5059040478 @default.
• W4205127744 creator A5073216448 @default.
• W4205127744 date "2022-01-18" @default.
• W4205127744 modified "2023-10-18" @default.
• W4205127744 title "Horizontal Fracture Formation in the Cenozoic Mudstone of the Western Qaidam Basin" @default.
• W4205127744 cites W1963766458 @default.
• W4205127744 cites W1983044633 @default.
• W4205127744 cites W1993697991 @default.
• W4205127744 cites W1997431460 @default.
• W4205127744 cites W2004339551 @default.
• W4205127744 cites W2007824856 @default.
• W4205127744 cites W2008643452 @default.
• W4205127744 cites W2016461253 @default.
• W4205127744 cites W2017332662 @default.
• W4205127744 cites W2029988410 @default.
• W4205127744 cites W2041999995 @default.
• W4205127744 cites W2043900361 @default.
• W4205127744 cites W2063908305 @default.
• W4205127744 cites W2066878990 @default.
• W4205127744 cites W2082503107 @default.
• W4205127744 cites W2092481183 @default.
• W4205127744 cites W2096140565 @default.
• W4205127744 cites W2105160961 @default.
• W4205127744 cites W2105325875 @default.
• W4205127744 cites W2114802403 @default.
• W4205127744 cites W2115518283 @default.
• W4205127744 cites W2133000084 @default.
• W4205127744 cites W2155128667 @default.
• W4205127744 cites W2167174628 @default.
• W4205127744 cites W4211087191 @default.
• W4205127744 cites W4254618661 @default.
• W4205127744 cites W4379466607 @default.
• W4205127744 doi "https://doi.org/10.3389/feart.2021.826124" @default.
• W4205127744 hasPublicationYear "2022" @default.
• W4205127744 type Work @default.
• W4205127744 citedByCount "1" @default.
• W4205127744 countsByYear W42051277442023 @default.
• W4205127744 crossrefType "journal-article" @default.
• W4205127744 hasAuthorship W4205127744A5017732563 @default.
• W4205127744 hasAuthorship W4205127744A5030452192 @default.
• W4205127744 hasAuthorship W4205127744A5040825987 @default.
• W4205127744 hasAuthorship W4205127744A5058749575 @default.
• W4205127744 hasAuthorship W4205127744A5059040478 @default.
• W4205127744 hasAuthorship W4205127744A5073216448 @default.
• W4205127744 hasBestOaLocation W42051277441 @default.
• W4205127744 hasConcept C109007969 @default.
• W4205127744 hasConcept C114793014 @default.
• W4205127744 hasConcept C116637073 @default.
• W4205127744 hasConcept C127313418 @default.
• W4205127744 hasConcept C139419234 @default.
• W4205127744 hasConcept C146357865 @default.
• W4205127744 hasConcept C151730666 @default.
• W4205127744 hasConcept C165205528 @default.
• W4205127744 hasConcept C43369102 @default.
• W4205127744 hasConcept C5900021 @default.
• W4205127744 hasConcept C77928131 @default.
• W4205127744 hasConcept C87432785 @default.
• W4205127744 hasConceptScore W4205127744C109007969 @default.
• W4205127744 hasConceptScore W4205127744C114793014 @default.
• W4205127744 hasConceptScore W4205127744C116637073 @default.
• W4205127744 hasConceptScore W4205127744C127313418 @default.
• W4205127744 hasConceptScore W4205127744C139419234 @default.
• W4205127744 hasConceptScore W4205127744C146357865 @default.
• W4205127744 hasConceptScore W4205127744C151730666 @default.
• W4205127744 hasConceptScore W4205127744C165205528 @default.
• W4205127744 hasConceptScore W4205127744C43369102 @default.
• W4205127744 hasConceptScore W4205127744C5900021 @default.
• W4205127744 hasConceptScore W4205127744C77928131 @default.
• W4205127744 hasConceptScore W4205127744C87432785 @default.
• W4205127744 hasFunder F4320321001 @default.
• W4205127744 hasLocation W42051277441 @default.
• W4205127744 hasLocation W42051277442 @default.
• W4205127744 hasOpenAccess W4205127744 @default.
• W4205127744 hasPrimaryLocation W42051277441 @default.
• W4205127744 hasRelatedWork W1965870423 @default.
• W4205127744 hasRelatedWork W2060229291 @default.
• W4205127744 hasRelatedWork W2347720059 @default.
• W4205127744 hasRelatedWork W2348087381 @default.
• W4205127744 hasRelatedWork W2374649853 @default.
• W4205127744 hasRelatedWork W2391363624 @default.
• W4205127744 hasRelatedWork W2393371679 @default.
• W4205127744 hasRelatedWork W4281698696 @default.
• W4205127744 hasRelatedWork W4295677999 @default.
• W4205127744 hasRelatedWork W816694438 @default.
• W4205127744 hasVolume "9" @default.
• W4205127744 isParatext "false" @default.
• W4205127744 isRetracted "false" @default.
• W4205127744 workType "article" @default.