FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W258507765> ?p ?o ?g. }

• W258507765 endingPage "38" @default.
• W258507765 startingPage "27" @default.
• W258507765 abstract "The texture and the grain composition of sandstone provide information about the tectonic setting of basins of deposition and associated provenances. The geological history of the Khangay-Khentey belt composed of pre-Carboniferous accretionary complex and Carboniferous shallow-marine strata was linked with the evolution of the Mongol-Okhotsk Ocean. This paper describes the sandstones of the Gorkhi, Altan-Ovoo & OrgiochUul Formations and Carboniferous shallow marine system, that occurs around Ulaanbaatar city The sandstones in the Gorkhi and Altan-Ovoo & Orgioch-Uul Formations are classified as feldspathic arenite. They are clast supported and poorly-sorted, with dominantly angular to very angular grains mainly composed of quartz, potassium feldspar, plagioclase and rock fragments of rhyolite and tuff. The modal framework grain analysis shows that sandy detritus was derived from “continental crust” where erosion has cut deep into volcanic cover. The sandstone in the Carboniferous shallow marine system classified as feldspathic wacke is rich in muddy matrix and poorly-sorted, dominantly includes rounded to little angular grains of quartz, potassium feldspar, plagioclase and rock fragments of rhyolite, felsic tuff, andesite and basalt. The Qm-F-Lt diagram suggests that the sandstone is originated from the “transitional arc”. The sandstones from the Gorkhi and Altan-Ovoo & Orgioch-Uul Formations are significantly similar and they can not be distinguished to each other in their textures, grain compositions and poor in rock fragments, and they were originated from the same kinds of source, i.e. continental crust where erosion has cut deep into volcanic cover which related to the subduction of oceanic plate. However, the lithostratigraphies of these formations are quite different each other and they were likely to have been formed at different places, or formed in different ages each other. The volcanism evidenced by the felsic tuff intercalations in the Altan-Ovoo & Orgioch-Uul Formation at the provenance area was likely enough immature which could not provide much volcanic rock fragments to the basin. The sandstone of the “Carboniferous formation,” rich in volcanic rock fragments, strongly indicates that the volcanic activity had developed to supply volcanic rock fragments into the sedimentary basin of this formation." @default.
• W258507765 created "2016-06-24" @default.
• W258507765 creator A5037060560 @default.
• W258507765 creator A5039908514 @default.
• W258507765 creator A5045161818 @default.
• W258507765 creator A5061608188 @default.
• W258507765 creator A5063896736 @default.
• W258507765 creator A5064817630 @default.
• W258507765 creator A5078111213 @default.
• W258507765 creator A5088628357 @default.
• W258507765 date "2012-12-25" @default.
• W258507765 modified "2023-09-23" @default.
• W258507765 title "Description of sandstones in the Ulaanbaatar area, Mongolia" @default.
• W258507765 cites W1978595079 @default.
• W258507765 cites W2008127132 @default.
• W258507765 cites W2042266298 @default.
• W258507765 cites W2055794724 @default.
• W258507765 cites W2060839901 @default.
• W258507765 cites W2075349472 @default.
• W258507765 cites W2081554454 @default.
• W258507765 cites W2089096123 @default.
• W258507765 cites W2106161981 @default.
• W258507765 cites W346871809 @default.
• W258507765 doi "https://doi.org/10.18999/bulnum.028.03" @default.
• W258507765 hasPublicationYear "2012" @default.
• W258507765 type Work @default.
• W258507765 sameAs 258507765 @default.
• W258507765 citedByCount "2" @default.
• W258507765 countsByYear W2585077652012 @default.
• W258507765 crossrefType "journal-article" @default.
• W258507765 hasAuthorship W258507765A5037060560 @default.
• W258507765 hasAuthorship W258507765A5039908514 @default.
• W258507765 hasAuthorship W258507765A5045161818 @default.
• W258507765 hasAuthorship W258507765A5061608188 @default.
• W258507765 hasAuthorship W258507765A5063896736 @default.
• W258507765 hasAuthorship W258507765A5064817630 @default.
• W258507765 hasAuthorship W258507765A5078111213 @default.
• W258507765 hasAuthorship W258507765A5088628357 @default.
• W258507765 hasConcept C109007969 @default.
• W258507765 hasConcept C113754120 @default.
• W258507765 hasConcept C12015391 @default.
• W258507765 hasConcept C120806208 @default.
• W258507765 hasConcept C127313418 @default.
• W258507765 hasConcept C138170599 @default.
• W258507765 hasConcept C141646446 @default.
• W258507765 hasConcept C149918038 @default.
• W258507765 hasConcept C151730666 @default.
• W258507765 hasConcept C17409809 @default.
• W258507765 hasConcept C192241223 @default.
• W258507765 hasConcept C193429443 @default.
• W258507765 hasConcept C25822816 @default.
• W258507765 hasConcept C2776698055 @default.
• W258507765 hasConcept C41440632 @default.
• W258507765 hasConcept C63376196 @default.
• W258507765 hasConcept C6494504 @default.
• W258507765 hasConceptScore W258507765C109007969 @default.
• W258507765 hasConceptScore W258507765C113754120 @default.
• W258507765 hasConceptScore W258507765C12015391 @default.
• W258507765 hasConceptScore W258507765C120806208 @default.
• W258507765 hasConceptScore W258507765C127313418 @default.
• W258507765 hasConceptScore W258507765C138170599 @default.
• W258507765 hasConceptScore W258507765C141646446 @default.
• W258507765 hasConceptScore W258507765C149918038 @default.
• W258507765 hasConceptScore W258507765C151730666 @default.
• W258507765 hasConceptScore W258507765C17409809 @default.
• W258507765 hasConceptScore W258507765C192241223 @default.
• W258507765 hasConceptScore W258507765C193429443 @default.
• W258507765 hasConceptScore W258507765C25822816 @default.
• W258507765 hasConceptScore W258507765C2776698055 @default.
• W258507765 hasConceptScore W258507765C41440632 @default.
• W258507765 hasConceptScore W258507765C63376196 @default.
• W258507765 hasConceptScore W258507765C6494504 @default.
• W258507765 hasIssue "28" @default.
• W258507765 hasLocation W2585077651 @default.
• W258507765 hasOpenAccess W258507765 @default.
• W258507765 hasPrimaryLocation W2585077651 @default.
• W258507765 hasRelatedWork W180273288 @default.
• W258507765 hasRelatedWork W1969290325 @default.
• W258507765 hasRelatedWork W1979393851 @default.
• W258507765 hasRelatedWork W1984302472 @default.
• W258507765 hasRelatedWork W1995968972 @default.
• W258507765 hasRelatedWork W2023233603 @default.
• W258507765 hasRelatedWork W2075918033 @default.
• W258507765 hasRelatedWork W2091652771 @default.
• W258507765 hasRelatedWork W2100643455 @default.
• W258507765 hasRelatedWork W2109873825 @default.
• W258507765 hasRelatedWork W2110048968 @default.
• W258507765 hasRelatedWork W2131043943 @default.
• W258507765 hasRelatedWork W2187799228 @default.
• W258507765 hasRelatedWork W2259459298 @default.
• W258507765 hasRelatedWork W2359246877 @default.
• W258507765 hasRelatedWork W2360799395 @default.
• W258507765 hasRelatedWork W2496969011 @default.
• W258507765 hasRelatedWork W50423620 @default.
• W258507765 hasRelatedWork W72816176 @default.
• W258507765 hasRelatedWork W1571005568 @default.
• W258507765 isParatext "false" @default.
• W258507765 isRetracted "false" @default.

• next