Matches in SemOpenAlex for { <https://semopenalex.org/work/W2955517225> ?p ?o ?g. }
- W2955517225 endingPage "276" @default.
- W2955517225 startingPage "261" @default.
- W2955517225 abstract "Abstract The Hacımahmutuşağı area (Aksaray/Turkey) is located in the western part of the Central Anatolian Crystalline Complex (CACC). Gneiss and marble compose the basement units, while intrusive rocks are gabbros and granitoids. The pegmatitic hornblende gabbros contain pegmatitic to fine-grained hornblendes, plagioclase, clinopyroxene, and accessory opaque minerals. The fine-grained gabbros, on the other hand, are composed of plagioclase, hornblende, and biotite as major components whereas the apatite and opaque minerals are present in accessory content. Granitic– granodioritic rocks are the common intrusive rock types in the area, and constitute quartz, orthoclase, plagioclase and biotite, and accessory zircon and opaque minerals. Leucogranites, comprising quartz, orthoclase, plagioclase with minor biotite, hornblende, and with accessory apatite and opaque minerals, are found as dykes intruding the marble and the granitic–granodioritic rocks. Strontium–neodymium isotope data of gabbros and granitoids have high 87 Sr/ 86 Sr (i) ratios (0.7076 to 0.7117) and low ɛNd (i) values (−5.0 to −9.8) point out enriched source and pronounced crustal contribution in their genesis. In the Hacımahmutuşağı area, it is plausible that the heat increase caused by the hot zone, which was generated by underplating mafic magma along with the hydrous mafic sills in the lower crust, might have resulted in partial melts from crystallized mafic sills and older crustal rocks. It can be suggested that these hybrid melts adiabatically rose to the shallow crust, ponded and crystallized there and formed the magma source of the intrusive rocks within the Hacımahmutuşağı area and the other hybrid granitic rocks with crustal signatures in the CACC. Geochemical data indicate that granitoids and gabbros are collision to post-collision related sub-alkaline rocks derived from an enriched source with extensive crustal inputs." @default.
- W2955517225 created "2019-07-12" @default.
- W2955517225 creator A5083229170 @default.
- W2955517225 date "2019-06-01" @default.
- W2955517225 modified "2023-09-27" @default.
- W2955517225 title "The Upper Cretaceous intrusive rocks with extensive crustal contribution in Hacımahmutuşağı Area (Aksaray/Turkey)" @default.
- W2955517225 cites W1514994218 @default.
- W2955517225 cites W1933180709 @default.
- W2955517225 cites W1969859799 @default.
- W2955517225 cites W1974501258 @default.
- W2955517225 cites W1977548506 @default.
- W2955517225 cites W1978049764 @default.
- W2955517225 cites W1983611242 @default.
- W2955517225 cites W1990305818 @default.
- W2955517225 cites W1992489808 @default.
- W2955517225 cites W1995857854 @default.
- W2955517225 cites W1999345020 @default.
- W2955517225 cites W2003419738 @default.
- W2955517225 cites W2004072968 @default.
- W2955517225 cites W2013491092 @default.
- W2955517225 cites W2014608018 @default.
- W2955517225 cites W2021987309 @default.
- W2955517225 cites W2023320566 @default.
- W2955517225 cites W2028453174 @default.
- W2955517225 cites W2029786633 @default.
- W2955517225 cites W2045719248 @default.
- W2955517225 cites W2058234247 @default.
- W2955517225 cites W2059439193 @default.
- W2955517225 cites W2080474021 @default.
- W2955517225 cites W2084673470 @default.
- W2955517225 cites W2086557360 @default.
- W2955517225 cites W2096896663 @default.
- W2955517225 cites W2099243038 @default.
- W2955517225 cites W2106501406 @default.
- W2955517225 cites W2108971421 @default.
- W2955517225 cites W2116357102 @default.
- W2955517225 cites W2120606565 @default.
- W2955517225 cites W2131104903 @default.
- W2955517225 cites W2138522501 @default.
- W2955517225 cites W2155604370 @default.
- W2955517225 cites W2155636239 @default.
- W2955517225 cites W2155791251 @default.
- W2955517225 cites W2161188118 @default.
- W2955517225 cites W2162613654 @default.
- W2955517225 cites W2164468447 @default.
- W2955517225 cites W2170189319 @default.
- W2955517225 cites W2286592209 @default.
- W2955517225 cites W2310440499 @default.
- W2955517225 cites W2343544986 @default.
- W2955517225 cites W2413911657 @default.
- W2955517225 cites W2520562807 @default.
- W2955517225 cites W2523077334 @default.
- W2955517225 cites W2895631292 @default.
- W2955517225 cites W2903066074 @default.
- W2955517225 cites W2940633697 @default.
- W2955517225 cites W857562136 @default.
- W2955517225 doi "https://doi.org/10.2478/geoca-2019-0015" @default.
- W2955517225 hasPublicationYear "2019" @default.
- W2955517225 type Work @default.
- W2955517225 sameAs 2955517225 @default.
- W2955517225 citedByCount "2" @default.
- W2955517225 countsByYear W29555172252022 @default.
- W2955517225 countsByYear W29555172252023 @default.
- W2955517225 crossrefType "journal-article" @default.
- W2955517225 hasAuthorship W2955517225A5083229170 @default.
- W2955517225 hasBestOaLocation W29555172251 @default.
- W2955517225 hasConcept C118270999 @default.
- W2955517225 hasConcept C120806208 @default.
- W2955517225 hasConcept C127313418 @default.
- W2955517225 hasConcept C151730666 @default.
- W2955517225 hasConcept C167284885 @default.
- W2955517225 hasConcept C17409809 @default.
- W2955517225 hasConcept C183222429 @default.
- W2955517225 hasConcept C195845463 @default.
- W2955517225 hasConcept C2777212541 @default.
- W2955517225 hasConcept C2777229588 @default.
- W2955517225 hasConcept C2778849375 @default.
- W2955517225 hasConcept C2779181077 @default.
- W2955517225 hasConcept C2779514672 @default.
- W2955517225 hasConcept C2779870107 @default.
- W2955517225 hasConcept C33757491 @default.
- W2955517225 hasConcept C42787717 @default.
- W2955517225 hasConcept C58097730 @default.
- W2955517225 hasConcept C5900021 @default.
- W2955517225 hasConcept C77928131 @default.
- W2955517225 hasConcept C79605941 @default.
- W2955517225 hasConceptScore W2955517225C118270999 @default.
- W2955517225 hasConceptScore W2955517225C120806208 @default.
- W2955517225 hasConceptScore W2955517225C127313418 @default.
- W2955517225 hasConceptScore W2955517225C151730666 @default.
- W2955517225 hasConceptScore W2955517225C167284885 @default.
- W2955517225 hasConceptScore W2955517225C17409809 @default.
- W2955517225 hasConceptScore W2955517225C183222429 @default.
- W2955517225 hasConceptScore W2955517225C195845463 @default.
- W2955517225 hasConceptScore W2955517225C2777212541 @default.
- W2955517225 hasConceptScore W2955517225C2777229588 @default.
- W2955517225 hasConceptScore W2955517225C2778849375 @default.
- W2955517225 hasConceptScore W2955517225C2779181077 @default.