Petrochemistry and Parent Rock Characteristics of the Amphibolites in the Gümüşler Formation of the Niğde Metamorphics, Central Turkey

Authors : K. Koçak, M. Arslan, H. Kurt, H. Baş, A. Döyen

Pages : 1-10

View : 24 | Download : 11

Publication Date : 2006-04-01

Article Type : Research

Abstract :In this study, it was attempted to determine the petrochcmistry and parent rock characteristics of the  Gümüşler amphibolites, associatcd with marble and quartzite, from the Niğde metamorplıics by using tlıcir  whole-rock chemical analyses. Amphibolites are associated with a seri es of Pre-Cretaceous supracmstal  metasediınents of the Gümüşler Formation. Massive and variably foliated amphibolites are made up mainly  by plagioclase, hornblende, quartz, diopsite witlı accessory sphene and apatite. Based on trace element  characteristics, the amphibolites are suggested to be metaigneous roeks; tuff or less likely basaltic-andesitic  lava/sili, which were emplaced between metasediınents. Their parent rocks are subalkalinc basalt and  andesite in cnmposition, and are characterisedby high K2O, Rb, Sr, Ba, K/Rb (-270-550) ratin, and lowMgO,  Ti,Y, Zr, CaO/Al2O3 ratio. Pctrochenıical dataalso suggcstthat the parent rocks of these ortho amphibolites  were possibly founded by fractional crystallization of olivine, clinopyroxene and hornblende.
Keywords : Amphibolite, Gümüşler Formation, Metamorphism, Niğde massif, Petrochemistry