Relationship between chemical composition and magnetic susceptibility in the alkaline volcanics from the Isparta area, SW Turkey

Abstract

Potassium-rich volcanic rocks in the Isparta area (SW Turkey) consist mainly of older (Pliocene) volcanic rock suites (e.g., lamprophyre, basaltic trachyandesite, trachyandesite, trachyte) and younger (Quaternary) caldera forming lava dome/flows (e.g., tephriphonolite, trachyte) and pyroclastics (ash/pumice fall deposits and ignimbritic flows). The magnetic susceptibility (K) was performed for both groups. The magnetic susceptibility value of the less evolved rocks characterized by SiO 2 < 57 wt% (e.g., basaltic trachyandesite, tephriphonolite, lamprophyric rocks) and having mostly mafic phenocrysts such as pyroxene, amphibole, and biotite-phlogopite is over 10 (10 −3 [SI]). Fine to medium-grained and subhedral to anhedral opaque minerals are scattered especially in the matrix phase of the less evolved volcanic rocks. However, the K value of the more evolved rocks (e.g., trachyte and trachyandesites) with SiO 2 over 57 wt% vary between 0.1 and 28, but most of them below 10. SI values are negatively correlated with SiO 2 , Na 2 O, but positively correlated with Fe 2 O 3 , CaO, MnO, P 2 O 5 and MgO contents, suggesting inverse variation of SI with fractionation of potassic magma. That is to say that less evolved volcanic rocks have relatively higher magnetic susceptibility values in the volcanic suite. Fine to medium-grained and subhedral to anhedral Fe-Ti oxides are scattered mainly in the matrix phase of the less evolved volcanics, presumably cause the pronounced relatively higher magnetic susceptibility.

Recognition of the Minoan tephra in the Acigöl Basin, western Turkey: implications for inter‐archive correlations and fine ash dispersal

“…Gölhisar data are from Elitok et al . (), Cappadocia data from Druitt et al . () and Minoan data from Eastwood et al .…”

“…Taking into account the rhyolitic composition of the tephra layer, sources from Gö lcü k and Kula volcanoes can be excluded, because their alkaline products never reached the rhyolitic field (Elitok et al, 2010). In turn, explosive products from Cappadocian volcanoes are too evolved (SiO 2 in excess of 75 wt%; Druitt et al, 1995;Develle et al, 2009;Hamann et al, 2010;Fig.…”