FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2022128630> ?p ?o ?g. }

• W2022128630 endingPage "262" @default.
• W2022128630 startingPage "240" @default.
• W2022128630 abstract "Miocene successions in western Turkey are dominated by lacustrine, fluvial and evaporitic sedimentary deposits. These deposits include considerable amounts of volcaniclastic detritus derived from numerous NE-trending volcanic centres in western Turkey as well as in the Bigadiç region. Early Miocene syn-depositional NE-trending olivine basalt and trachyandesite bodies that formed as intrusions and lava flows occur within the Bigadiç borate basin. Olivine basalts occur as partly emergent intrusions, and trachyandesite dykes fed extensive lava flows emplaced in a semi-arid lacustrine environment. Peperites associated with the olivine basalt and trachyandesites appear to display contrasting textural features, although all the localities include a large variety of clast morphologies from blocky to fluidal. Fluidal clasts, mainly globular, ameboidal and pillow-like varieties, are widespread in the peperite domains associated with olivine basalts, apparently due to large-volume sediment fluidisation. In contrast, fluidal clasts related to trachyandesites are restricted to narrow zones near the margins of the intrusions and have commonly elongate and polyhedral shapes with digitate margins, rather than globular and equant varieties. Blocky and fluidal clasts in the olivine basalt peperite display progressive disintegration, suggesting decreasing temperature and increasing viscosity during fragmentation. Abundance of blocky clasts with respect to fluidal clasts in the trachyandesite peperite indicates that the fluidal emplacement and low-volume sediment fluidisation in the early stages were immediately followed by quench fragmentation due to the high viscosity of the magma. Size, texture and abundance of the blocky and fluidal clasts in the olivine basalt and trachyandesite peperites were mainly controlled by sediment fluidisation, pulsatory magma injection and magma properties such as composition, viscosity, vesicularity, and size, abundance and orientation of phenocrysts. Variously combining these contrasting features to varying degrees may form diverse juvenile clast shapes in peperitic domains." @default.
• W2022128630 created "2016-06-24" @default.
• W2022128630 creator A5056135164 @default.
• W2022128630 creator A5060548690 @default.
• W2022128630 creator A5072894480 @default.
• W2022128630 date "2006-01-01" @default.
• W2022128630 modified "2023-10-17" @default.
• W2022128630 title "Olivine basalt and trachyandesite peperites formed at the subsurface/surface interface of a semi-arid lake: An example from the Early Miocene Bigadiç basin, western Turkey" @default.
• W2022128630 cites W1965919385 @default.
• W2022128630 cites W1969556063 @default.
• W2022128630 cites W1969670016 @default.
• W2022128630 cites W1971619354 @default.
• W2022128630 cites W1983926551 @default.
• W2022128630 cites W1989323149 @default.
• W2022128630 cites W1994935981 @default.
• W2022128630 cites W1995574789 @default.
• W2022128630 cites W1997952954 @default.
• W2022128630 cites W1998032495 @default.
• W2022128630 cites W1999448338 @default.
• W2022128630 cites W2009731963 @default.
• W2022128630 cites W2009900924 @default.
• W2022128630 cites W2014477862 @default.
• W2022128630 cites W2015832188 @default.
• W2022128630 cites W2023687051 @default.
• W2022128630 cites W2030907220 @default.
• W2022128630 cites W2032827003 @default.
• W2022128630 cites W2035268287 @default.
• W2022128630 cites W2035548027 @default.
• W2022128630 cites W2042937799 @default.
• W2022128630 cites W2044813446 @default.
• W2022128630 cites W2044878300 @default.
• W2022128630 cites W2045594539 @default.
• W2022128630 cites W2049608724 @default.
• W2022128630 cites W2054008241 @default.
• W2022128630 cites W2057686652 @default.
• W2022128630 cites W2063486652 @default.
• W2022128630 cites W2065192273 @default.
• W2022128630 cites W2067875518 @default.
• W2022128630 cites W2073888430 @default.
• W2022128630 cites W2076628956 @default.
• W2022128630 cites W2079946929 @default.
• W2022128630 cites W2090537205 @default.
• W2022128630 cites W2090888922 @default.
• W2022128630 cites W2092690171 @default.
• W2022128630 cites W2098447346 @default.
• W2022128630 cites W2100938899 @default.
• W2022128630 cites W2103141690 @default.
• W2022128630 cites W2103423405 @default.
• W2022128630 cites W2103655185 @default.
• W2022128630 cites W2115164451 @default.
• W2022128630 cites W2115550380 @default.
• W2022128630 cites W2117996530 @default.
• W2022128630 cites W2144132578 @default.
• W2022128630 cites W2148064881 @default.
• W2022128630 cites W2161182422 @default.
• W2022128630 cites W2168380098 @default.
• W2022128630 cites W2169326720 @default.
• W2022128630 cites W32303315 @default.
• W2022128630 cites W4239634001 @default.
• W2022128630 doi "https://doi.org/10.1016/j.jvolgeores.2005.07.016" @default.
• W2022128630 hasPublicationYear "2006" @default.
• W2022128630 type Work @default.
• W2022128630 sameAs 2022128630 @default.
• W2022128630 citedByCount "25" @default.
• W2022128630 countsByYear W20221286302012 @default.
• W2022128630 countsByYear W20221286302013 @default.
• W2022128630 countsByYear W20221286302014 @default.
• W2022128630 countsByYear W20221286302015 @default.
• W2022128630 countsByYear W20221286302016 @default.
• W2022128630 countsByYear W20221286302017 @default.
• W2022128630 countsByYear W20221286302018 @default.
• W2022128630 countsByYear W20221286302019 @default.
• W2022128630 countsByYear W20221286302020 @default.
• W2022128630 countsByYear W20221286302021 @default.
• W2022128630 crossrefType "journal-article" @default.
• W2022128630 hasAuthorship W2022128630A5056135164 @default.
• W2022128630 hasAuthorship W2022128630A5060548690 @default.
• W2022128630 hasAuthorship W2022128630A5072894480 @default.
• W2022128630 hasConcept C113754120 @default.
• W2022128630 hasConcept C120806208 @default.
• W2022128630 hasConcept C127313418 @default.
• W2022128630 hasConcept C138170599 @default.
• W2022128630 hasConcept C161509811 @default.
• W2022128630 hasConcept C167284885 @default.
• W2022128630 hasConcept C17409809 @default.
• W2022128630 hasConcept C192241223 @default.
• W2022128630 hasConcept C2780364934 @default.
• W2022128630 hasConcept C5900021 @default.
• W2022128630 hasConcept C6494504 @default.
• W2022128630 hasConcept C95869378 @default.
• W2022128630 hasConceptScore W2022128630C113754120 @default.
• W2022128630 hasConceptScore W2022128630C120806208 @default.
• W2022128630 hasConceptScore W2022128630C127313418 @default.
• W2022128630 hasConceptScore W2022128630C138170599 @default.
• W2022128630 hasConceptScore W2022128630C161509811 @default.
• W2022128630 hasConceptScore W2022128630C167284885 @default.
• W2022128630 hasConceptScore W2022128630C17409809 @default.
• W2022128630 hasConceptScore W2022128630C192241223 @default.

• next