Multidisciplinary Insights into Zeolite and Clay Formation in Hydrothermally Altered Volcanic Rocks of Cubuk, Turkey

Abstract

The present study addressed the influence of lithological variability on hydrothermal alteration processes in the Cubuk region of Ankara, recognized globally for its agate occurrences. The objective was to clarify how differing host rocks, tuff and ignimbrite in Karadana, and perlitic units in Yukariemirler, affect secondary mineral formation and alteration pathways. A combination of mineralogical (X-ray diffraction, Fourier-transform infrared spectroscopy, field-emission scanning electron microscopy) and geochemical (energy-dispersive X-ray spectroscopy, whole-rock geochemistry, delta O-18-delta D) methods was utilized to characterize alteration assemblages and fluid conditions. The alteration sequence progressed through five stages, beginning with unaltered volcanic rocks. In the second stage, smectite-group clays, particularly montmorillonite, were formed under mildly alkaline and low-temperature conditions (pH 7.5-9.0; T 43-50 degrees C). This initial clay formation was followed by zeolitization along two distinct pathways: clinoptilolite crystallized (K-rich, Si/Al similar to 4.2) in the Karadana tuff-ignimbrite units, while heulandite formed (Ca-rich, Si/Al similar to 2.7) in the perlitic host rocks of Yukariemirler. These variations are attributed to differences in host-rock composition, permeability, and hydrothermal fluid chemistry. In more advanced stages, mordenite and chabazite precipitated under progressively higher pH and temperature conditions (pH 9.5-10.0; T 70-80 degrees C). In the final stage, opal-quartz formed due to silica supersaturation triggered by a drop in pH, despite rising temperatures (pH similar to 8.5-9.0; T similar to 250 degrees C). The paragenetic sequence confirms that clay mineral formation preceded zeolitization in both zones. Variations in zeolite types reflect strong lithological and hydrochemical controls, as well as the origin of the hydrothermal fluids; clinoptilolite formation in Karadana is associated with Na- and K-rich supergene fluids, while Ca-rich hypogene fluids promoted heulandite precipitation in Yukariemirler. This study presents the first detailed paragenetic model for zeolite-clay alteration in the Cubuk volcanic system and offers new insights into post-caldera hydrothermal evolution in Central Anatolia.