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Fossil geothermal systems in the continental rift zone of the Kucuk Menderes within the Menderes Massif, Western Anatolia, Turkey

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dc.creator Ozgur, Nevzat
dc.date 2001-01-01T01:00:00Z
dc.date.accessioned 2021-12-03T11:29:52Z
dc.date.available 2021-12-03T11:29:52Z
dc.identifier 6745cf1a-9d54-4d18-b349-3650a42daf19
dc.identifier https://avesis.sdu.edu.tr/publication/details/6745cf1a-9d54-4d18-b349-3650a42daf19/oai
dc.identifier.uri http://acikerisim.sdu.edu.tr/xmlui/handle/123456789/92308
dc.description The Hg, Sb and Au deposits of Halikoy, Emirli and Kure can be considered as fossil equivalents of formerly active geothermal systems due to various similarities of parameters. The metals originated in the host rocks were transported in a hydrothermal system as (HS)(2)(-) complexes. The precipitation of metals depended upon T, P, pH and redox potential as well as total sulfur concentration.
dc.language eng
dc.rights info:eu-repo/semantics/closedAccess
dc.title Fossil geothermal systems in the continental rift zone of the Kucuk Menderes within the Menderes Massif, Western Anatolia, Turkey
dc.type info:eu-repo/semantics/conferenceObject


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