Tectonic settings of porphyry-type mineralization and hydrothermal alteration in Paleozoic island arcs and active continental margins, Kyrghyz Range, (Tien Shan) Kyrghyzstan |
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Authors: | R J Jenchuraeva |
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Institution: | (1) Geological Institute of Academy of Science, Erkindik str.30. Republic of Kyrghyzstan, XX |
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Abstract: | Ore deposits in the fold belts of the northern Tien Shan have been formed in two stages and occur in two types of tectonic
settings. The first type is represented by Early Ordovician island arcs hosting the Karakol ore district. These east–west
trending island arcs are interpreted to have evolved above the south dipping subduction of oceanic crust of the Central Asian
paleo-ocean. The second type of tectonic setting hosting the Octorkoy Ore District, has evolved on a Devonian-Carboniferous
active continental margin of the Central Asian paleo-ocean above north dipping subduction of the oceanic crust. The second
type is superposed on the first tectonic setting. The Oktorkoy ore district is characterized by thrusting and similar circular
structures as in the first stage and its polygenic mineralization is associated with multiphase granitoid complexes. Zonality
of porphyry copper deposits of the Kyrghyz Range is associated with the following hydrothermal alteration sequence: potassium
alteration - phyllization (beresitization) - prophyllitization (epidote-chlorite-albite) - tourmalinization - argillization
- prophyllitization (epidote-actinolite-albite).
Received: 3 June 1996 / Accepted: 10 January 1997 |
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