dc.contributor.author | Alpaslan, M | |
dc.contributor.author | Yilmaz, H | |
dc.contributor.author | Temel, A | |
dc.date.accessioned | 2019-07-27T12:10:23Z | |
dc.date.accessioned | 2019-07-28T10:22:27Z | |
dc.date.available | 2019-07-27T12:10:23Z | |
dc.date.available | 2019-07-28T10:22:27Z | |
dc.date.issued | 2004 | |
dc.identifier.issn | 1335-0552 | |
dc.identifier.issn | 1336-8052 | |
dc.identifier.uri | https://hdl.handle.net/20.500.12418/11125 | |
dc.description | WOS: 000226356100006 | en_US |
dc.description.abstract | The Pliocene-Quaternary Karasar basalt is located in the western part of the post-collisional volcanic field in Eastern Anatolia and occurs as lava flows on the continental sediments. According to normative mineralogy and geochemistry, Karasar basalt samples have hyperstene-normative tholeiites, nepheline-normative basalts. trachybasalts and basaltic andesites with quartz-xenocrysts which occur at the base of the lava flows. Trace and rare element variations indicate that the trachybasalts are enriched in highly incompatible trace and light-rare earth elements relative to hyprstene-and nepheline-normative basalts. Hy-normative tholeiites have higher concentrations of medium-heavy rate earth elements relative to ne-normative basalts and trachybasalts. The trace element characteristics of the Karasar basalt imply that the quartz-bearing rocks indicate some crustal contributions, but the basaltic sampler, have a minimal or no crustal assimilation. Th/Yb-Nb/Yb and Hf/Sm-N-Ta/La-N diagrams coupled with HFSE depletions display a subduction signature in the source region of these volcanics. REE modeling exhibits that the magmas forming the Karasar basalt originated from a spinel-peridotite source, although trachybasalts require mixing between melts from spinel- and garnei-peridocite source. Discrimination plots based on trace element data exhibit a within-plate character of the Karasar basahs- Correlations between trace element ratios (Ba/Nb-La/Nb and Ba/La-Ce/Pb) imply that the source of Karasar basalt L, lithotspheric rather than the asthenospheric mantle. These data reveal that the Karasar basalt is linked to a posi-collisional extensional tectonic regime following the collision between the Eurasian and Arabian plates. Volcanism in this pan of Anatolia is consistent with a model in which melting of lithospheric mantle occurred in response to lithospheric extension. | en_US |
dc.language.iso | eng | en_US |
dc.publisher | SLOVAK ACAD SCIENCES GEOLOGICAL INST | en_US |
dc.rights | info:eu-repo/semantics/closedAccess | en_US |
dc.subject | Eastern Anatolia | en_US |
dc.subject | within-plate | en_US |
dc.subject | extensional | en_US |
dc.subject | post-collision | en_US |
dc.subject | alkaline | en_US |
dc.subject | tholeiitic | en_US |
dc.subject | petrology | en_US |
dc.title | Geochemistry of post-collision Pliocene-Quaternary Karasar basalt (Divrigi-Sivas, Eastern Turkey): Evidence for partial melting processes | en_US |
dc.type | article | en_US |
dc.relation.journal | GEOLOGICA CARPATHICA | en_US |
dc.contributor.department | Mersin Univ, Dept Geol, TR-33343 Mersin, Turkey -- Cumhuriyet Univ, Dept Geophys, TR-58140 Sivas, Turkey -- Hacettepe Univ, Dept Geol, TR-06532 Ankara, Turkey | en_US |
dc.contributor.authorID | Temel, Abidin -- 0000-0002-8051-4065 | en_US |
dc.identifier.volume | 55 | en_US |
dc.identifier.issue | 6 | en_US |
dc.identifier.endpage | 500 | en_US |
dc.identifier.startpage | 487 | en_US |
dc.relation.publicationcategory | Makale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı | en_US |