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Origin of Kaolin Deposits: Evidence From the Hisarcık (Emet-Kütahya) Deposits, Western Turkey
Alunite Hisarcı k hydrothermal alteration kaolinite Kütahya Natroalunite Smectite silica zone (silica gossan)
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2009/7/7
Kaolin deposits, situated approximately 20 km south of Hisarcık, have been formed by the alteration of dacite and dacitic tuffs related to the Miocene volcanism associated with extensional tecton...