Interpretation of the Magma Chamber Processes with the help of Textural Stratigraphy of the Plagioclases (Konya-Central Anatolia)

The variations in the chemical composition and micro-texture of a mineral from core to rim allow sequencing formation magma chamber processes interpretation which texture might have been formed by process. In this study, textural zoning plagioclases, are significant recorder processes, some enclave-containing andesite (calc-alkaline) basalts Karapınar Karacadağ Volcanic Complex, were examined their stratigraphies created enlight processes. Plagioclases enclave bearing andesites enclaves same andesine-bitovnite (An34-An75) composition. It is noteworthy that plagioclases host-rock mostly rounded, reverse oscillatory zoned with Fe, Mg, An, Sr, Ba. However they display generally fine sieve dusty texture. Plagioclase micro-phenocrysts calc-alkaline andesine-labrador (An32-An66) core-to-rim, suggesting may be xenocrysts rather than phenocrysts. Remarkably, show Ba, as well exhibit coarse-grained glass microlithic inclusions, spongy cellular textures. Considering properties basaltic rocks, decompression addition mixing (magma mixing/self-mixing) also affect genesis basalts. However, andesitic replenishment key role or temperature-pressure change.