Results 1 to 4 of about 7 (4)
Bulletin of the Mineral Research and Exploration, 2013 Şaphane bölgesinde temeli, Menderes masifinin kuzey kenarına ait Paleozoik yaşlı gnays, şist ve mermerler oluşturur. Bu temel kayaçlar Kretase yaşlı Dağardı ofiyolitik melanjı tarafından tektonik olarak üzerlenmektedir.
Musa BURÇAK +2 more
doaj +3 more sources
Mineralogy, geochemistry, and diagenesis of clinoptilolite tuffs (Miocene) in the central Simav graben, western Turkey [PDF]
, 2008 Miocene rifting and associated rhyolitic (K-rich) volcanism resulted in the deposition of pyroclastic material in the central Simav graben, near Karacaderbent, Turkey. The pyroclastics were deposited in a lacustrine environment, altered to clinoptilolite-
Elsen, Jan +5 more
core +3 more sources
, 2013 The basement in Şaphane region is constituted by Paleozoic gneiss, schist and marbles belonging to northern margin of the Menderes Massif. These basement rocks are overlain by Cretaceous aged Dağardı ophiolitic melange.
BURÇAK, Musa +2 more
core
Some of the next articles are maybe not open access.
2012
The basement in Şaphane region is constituted by Paleozoic gneiss, schist and marbles belonging to northern margin of the Menderes Massif. These basement rocks are overlain by Cretaceous aged Dağardı ophiolitic melange. All these rocks are discordantly covered by Neogene – Quaternary sedimentary and volcanic rocks deposited under lacustrine ...
BURÇAK, Musa +2 more
openaire +1 more source
The basement in Şaphane region is constituted by Paleozoic gneiss, schist and marbles belonging to northern margin of the Menderes Massif. These basement rocks are overlain by Cretaceous aged Dağardı ophiolitic melange. All these rocks are discordantly covered by Neogene – Quaternary sedimentary and volcanic rocks deposited under lacustrine ...
BURÇAK, Musa +2 more
openaire +1 more source