FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2894593134> ?p ?o ?g. }

• W2894593134 endingPage "65" @default.
• W2894593134 startingPage "27" @default.
• W2894593134 abstract "Late Cretaceous Chalk sedimentation history across the British Isles included (i) fault controlled uplift and subsidence in Northern Ireland and the Inner Hebrides and (ii) uplift along the lines of en echelon folds in Southern Britain and northern France. Synsedimentary slump folds and downslope displacement structures are compared with penecontemporaneous interbed slides and later tectonic folds and faults. Compressional strike-slip tectonic processes at Flamborough Head, Yorkshire, illustrate intra-Chalk slump beds in a half-graben setting. Progressive ‘growth’ of structures characterises early downslope slump folding, interbed sliding and some listric faulting. Sheet-flints replacing slide shear planes and early fractures provide evidence for early movements. Availability of open-slopes or the depth of burial under which the range of structures developed is reflected in the degree of disruption and fragmentation of chalk and flint. Fragmentation provides clues to the timing of events and origin of the Late Campanian Altachuile Breccia (Northern Ireland) and the Coniacian Hope Gap slides (Sussex). Fragmentation and formation of sheet flints together help distinguish intra-Chalk tectonics from Quaternary glacitectonic structures. The role of marl seams, high porosity chalk beds and hardgrounds on bed-sliding, décollement zones and disruption of chalk blocks from bedrock in glacitectonics is discussed. Chalk formations with marl seams develop a special style of fracturing related to early interbed sliding and pore-fluid escape structures. Marl-seams are shown to be primary sedimentary features and not the products of post depositional pressure-solution. More than any other formation the Late Santonian – Early Campanian Newhaven Chalk contains extensive sheet-flints and shows great lateral variation in thickness and lithology across the fold belts of southern England and northern France." @default.
• W2894593134 created "2018-10-12" @default.
• W2894593134 creator A5074984493 @default.
• W2894593134 date "2019-02-01" @default.
• W2894593134 modified "2023-10-14" @default.
• W2894593134 title "Late Cretaceous to Miocene and Quaternary deformation history of the Chalk: Channels, slumps, faults, folds and glacitectonics" @default.
• W2894593134 cites W1568329164 @default.
• W2894593134 cites W1587486956 @default.
• W2894593134 cites W1963643588 @default.
• W2894593134 cites W1966300379 @default.
• W2894593134 cites W1968084560 @default.
• W2894593134 cites W1968308617 @default.
• W2894593134 cites W1968940903 @default.
• W2894593134 cites W1970813250 @default.
• W2894593134 cites W1971323166 @default.
• W2894593134 cites W1973720657 @default.
• W2894593134 cites W1975702408 @default.
• W2894593134 cites W1977114195 @default.
• W2894593134 cites W1979412938 @default.
• W2894593134 cites W1988624279 @default.
• W2894593134 cites W1989763349 @default.
• W2894593134 cites W1994145711 @default.
• W2894593134 cites W1996446577 @default.
• W2894593134 cites W1997475287 @default.
• W2894593134 cites W2000366359 @default.
• W2894593134 cites W2002161968 @default.
• W2894593134 cites W2005297899 @default.
• W2894593134 cites W2006325910 @default.
• W2894593134 cites W2014456844 @default.
• W2894593134 cites W2016117888 @default.
• W2894593134 cites W2026771056 @default.
• W2894593134 cites W2027147592 @default.
• W2894593134 cites W2032038576 @default.
• W2894593134 cites W2034581644 @default.
• W2894593134 cites W2040750694 @default.
• W2894593134 cites W2043258475 @default.
• W2894593134 cites W2049729825 @default.
• W2894593134 cites W2051882950 @default.
• W2894593134 cites W2053139688 @default.
• W2894593134 cites W2060466463 @default.
• W2894593134 cites W2061245874 @default.
• W2894593134 cites W2061680126 @default.
• W2894593134 cites W2063188917 @default.
• W2894593134 cites W2065787090 @default.
• W2894593134 cites W2069407025 @default.
• W2894593134 cites W2069420671 @default.
• W2894593134 cites W2075037648 @default.
• W2894593134 cites W2075948222 @default.
• W2894593134 cites W2078935214 @default.
• W2894593134 cites W2082172259 @default.
• W2894593134 cites W2082410625 @default.
• W2894593134 cites W2096548164 @default.
• W2894593134 cites W2097947604 @default.
• W2894593134 cites W2098087841 @default.
• W2894593134 cites W2099614110 @default.
• W2894593134 cites W2107817958 @default.
• W2894593134 cites W2108196401 @default.
• W2894593134 cites W2108449782 @default.
• W2894593134 cites W2109328734 @default.
• W2894593134 cites W2109402692 @default.
• W2894593134 cites W2112583874 @default.
• W2894593134 cites W2133616354 @default.
• W2894593134 cites W2133882833 @default.
• W2894593134 cites W2150181750 @default.
• W2894593134 cites W2164737407 @default.
• W2894593134 cites W2169985658 @default.
• W2894593134 cites W2189218373 @default.
• W2894593134 cites W2332263366 @default.
• W2894593134 cites W2608207292 @default.
• W2894593134 cites W2790582937 @default.
• W2894593134 cites W3153317005 @default.
• W2894593134 cites W4253530491 @default.
• W2894593134 doi "https://doi.org/10.1016/j.pgeola.2018.01.004" @default.
• W2894593134 hasPublicationYear "2019" @default.
• W2894593134 type Work @default.
• W2894593134 sameAs 2894593134 @default.
• W2894593134 citedByCount "11" @default.
• W2894593134 countsByYear W28945931342019 @default.
• W2894593134 countsByYear W28945931342020 @default.
• W2894593134 countsByYear W28945931342021 @default.
• W2894593134 countsByYear W28945931342022 @default.
• W2894593134 countsByYear W28945931342023 @default.
• W2894593134 crossrefType "journal-article" @default.
• W2894593134 hasAuthorship W2894593134A5074984493 @default.
• W2894593134 hasConcept C109007969 @default.
• W2894593134 hasConcept C114793014 @default.
• W2894593134 hasConcept C12294951 @default.
• W2894593134 hasConcept C127313418 @default.
• W2894593134 hasConcept C127413603 @default.
• W2894593134 hasConcept C146588470 @default.
• W2894593134 hasConcept C151730666 @default.
• W2894593134 hasConcept C17409809 @default.
• W2894593134 hasConcept C53942344 @default.
• W2894593134 hasConcept C6494504 @default.
• W2894593134 hasConcept C77928131 @default.
• W2894593134 hasConcept C78519656 @default.
• W2894593134 hasConcept C92927620 @default.
• W2894593134 hasConceptScore W2894593134C109007969 @default.

• next