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Sökning: id:"swepub:oai:DiVA.org:ltu-77781" > Temporal, geochemic...

Temporal, geochemical and geodynamic evolution of the Late Cretaceous subduction zone volcanism in the eastern Sakarya Zone, NE Turkey : Implications for mantle-crust interaction in an arc setting

Aydin, Faruk (författare)
Karadeniz Technical University, Department of Geological Engineering
Saka, Simge Oguz (författare)
Karadeniz Technical University, Department of Geological Engineering
Sen, Cüneyt (författare)
Karadeniz Technical University, Department of Geological Engineering
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Dokuz, Abdurrahman (författare)
Gümüşhane University, Department of Geological Engineering
Aiglsperger, Thomas (författare)
Luleå tekniska universitet,Geovetenskap och miljöteknik
Uysal, Ibrahim (författare)
Karadeniz Technical University, Department of Geological Engineering
Kandemir, Raif (författare)
Recep Tayyip Erdoğan University, Department of Geological Engineering
Karsli, Orhan (författare)
Recep Tayyip Erdoğan University, Department of Geological Engineering
Sari, Bilal (författare)
Dokuz Eylül University, Department of Geological Engineering
Baser, Rasim (författare)
Karadeniz Technical University, Department of Geological Engineering
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 (creator_code:org_t)
Elsevier, 2020
2020
Engelska.
Ingår i: Journal of Asian Earth Sciences. - : Elsevier. - 1367-9120 .- 1878-5786. ; 192
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • The Late Cretaceous Artvin volcanic rocks (LCAVs) from the eastern Sakarya zone (ESZ) of NE Turkey are composed of mafic/basaltic (S1-Çatak and S2-Çağlayan) and felsic/acidic (S1-Kızılkaya and S2-Tirebolu) rock types that occurred in two successive stages: (i) first stage (S1: Turonian–Early Santonian) and (ii) second stage (S2: Late Santonian–Campanian). Clinopyroxene thermobarometric results point that the S2-Çağlayan basaltic rocks have crystallised at higher temperatures and under deeper crustal conditions than those of the S1-Çatak basaltic rocks.The LCAVs show a wide compositional spectrum, ranging from tholeiite to calc-alkaline/shoshonite and are typically represented by a geochemical composition resembling subduction-related arc rocks although the 87Sr/86Sr(i) (0.7044–0.7071) and ɛNd(i) values (−0.63 to + 3.47) as well as 206Pb/204Pb(i) (18.07–18.56), 207Pb/204Pb(i) (15.57–15.62) and 208Pb/204Pb(i) (37.12–38.55) ratios show very limited variation. The parent magmas of the S1-Çatak and S2-Çağlayan mafic volcanic rocks were derived from underplated basaltic melts that originated by partial melting of metasomatised spinel lherzolite and spinel-garnet lherzolite, respectively. It is proposed that the compositions of the S1-Kızılkaya (mainly dacitic) and S2-Tirebolu (rhyolitic to trachytic) felsic rocks were particularly controlled by metasomatised mantle–crust interaction and MASH zone + shallow crustal fractionation processes. Our data, together with data from previous studies, suggest that the S1- and S2-mafic and felsic rocks of the LCAVs (~95–75 Ma) are the products of two-stage volcanic event that took place during the northward subduction of the northern Neotethys Ocean (NNO).

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geokemi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geochemistry (hsv//eng)

Nyckelord

Late Cretaceous
Subduction
Volcanism
Mantle–crust interaction
Sakarya Zone
Eastern Pontides
NE Turkey
Applied Geochemistry
Tillämpad geokemi

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