TY - JOUR TT - Alkali-Silica Reaction Potential of Arc-related Volcanic Rocks from the Göksun Ophiolite (Kahramanmaraş-Turkey) AU - Rızaoğlu, Tamer PY - 2017 DA - April JF - Afyon Kocatepe Üniversitesi Fen Ve Mühendislik Bilimleri Dergisi PB - Afyon Kocatepe Üniversitesi WT - DergiPark SN - 2149-3367 SP - 247 EP - 256 VL - 17 IS - 1 LA - en KW - Ophiolite; volcanic KW - aggregate KW - Alkali-silica reactivity KW - Accelerated mortar bar method N2 - The alkali-silica reactivity is one of the most important problems that can occur in concrete structures.Because of their wide spectrum of mineralogical compositions and phases, volcanic rocks are morelikely to cause alkali-silica reactivity. In this study, alkali-silica reactivity potentials of the rocksrepresenting the upper levels of the crustal section of the Late Cretaceous suprasubduction-typeGöksun ophiolite in the Tauride ophiolitic belt have been investigated. The Göksun ophiolite displaysand intact ophiolite pseudostratigraphy with the thick layer of volcanic section characterized by adifferent composition of rock units such as basalt, basaltic-andesite, andesite, dacite and rhyolite.Firstly, the petrographic determinations of the samples derived from these volcanic units were madeand then geochemical analyzes carried o ut o n t he s ame s pecimens t o c ontrol t he a ccuracy o f t hepetrographic analyzes and the rocks were classified according to trace elements. Finally, theaccelerated mortar bar method was applied on the concrete bars produced from same rock samples tocompare the variation of Alkali-Silica Reactivity (ASR) with lithology. The test results yielded that theintermediate volcanics have much Alkali Silica Reactivity (ASR) potential than basic and acidic volcanics(basalts, rhyolites and dacites). It is estimated that the glassy matrix of the intermediate volcanics ispartly responsible for the alkali-silica reactivity. 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