Petrology of the late Triassic mafic volcanic rocks from the Antalya Complex, southern Turkey: evidence for mantle source characteristics during the Neotethyan rifting

Authors : Utku BAGCİ, Tamer RİZAOGLU, Guzide ONAL, Osman PARLAK

Pages : 1049-1072

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Publication Date : 0000-00-00

Article Type : Research Paper

Abstract :The Antalya Complex in southern Turkey comprises a number of autochthonous and allochthonous units that originated from the Southern Neotethys. Late Triassic volcanic rocks are widespread in the Antalya Complex and are important for the onset of the rifting stage of the southern Neotethys. The studied Late Triassic volcanic rocks within the Antalya Complex are exposed in the southern part of Saldikent insert ignore into journalissuearticles values(Antalya); region. They are represented by pillow, massive, and columnar-jointed lava flows with volcaniclastic breccias and pelagic limestone intercalations. Spilitic basalts exhibit intersertal, microlithic porphyritic, and ophitic textures and are represented by plagioclase, pyroxene, and olivine. Secondary phases are characterized by serpentine, calcite, chlorite, epidote, zeolite, and quartz. Based on Zr/Ti vs. Nb/Y ratios, the volcanic rocks are represented by alkaline basalts insert ignore into journalissuearticles values(Nb/Y = 1.54-2.82);. A chondrite normalized REE diagram for the volcanic rocks displays significant LREE enrichment with respect to HREE insert ignore into journalissuearticles values([La/Yb]insert ignore into journalissuearticles values(N); = 15.14-19.77);. Trace element geochemistry of the studied rocks suggests that these rocks are more akin to ocean island basalt insert ignore into journalissuearticles values(OIB); and were formed by small degrees insert ignore into journalissuearticles values(similar to 2-4%); of partial melting of an enriched mantle source insert ignore into journalissuearticles values(spinel + garnet-bearing lherzolite);. The volcanic rocks of the Saldikent region exhibit similarities to the Late Triassic volcanics of the Kocali Complex in SE Anatolia and the Mamonia Complex insert ignore into journalissuearticles values(Cyprus); in terms of their geochemical features. All evidence suggests that the Late Triassic alkaline volcanics in Antalya, Mamonia insert ignore into journalissuearticles values(Cyprus);, and the Kocali insert ignore into journalissuearticles values(Adiyaman); Complexes were formed in an extensional environment at the continent-ocean transition zone during the rifting of the southern Neotethyan Ocean.
Keywords : Alkali basalt, seamount, ΔNb, enriched mantle, Neotethys, Antalya Complex