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RELATION BETWEEN BASIC AND ACID MAGMATISM IN TIN-BEARING AREAS OF EASTERN YAKUTIA

Vera Trunilina

First published: 2018-06-20https://doi.org/10.5593/sgem2018/1.1/s01.073View metrics

Abstract

The article concentrates on relation of mineralization, granitoid magmatism and dikes in ore fields of the Eastern Yakutia with cassiterite-sulfide mineralization. It is shown that, the main ore bodies are confined to places of intensive development of dikes and do not significantly concur with the time of granitoid formation. The melts that formed dikes and generated into metasomatised mantle, was the main source of tin and accompanying elements. When centers of granitoid and dike eruption are the same, these melts were additional sources of heat and volatile components, that provided duration of granite system evolution and additional mobilization of ore material.

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Publication details

Title
RELATION BETWEEN BASIC AND ACID MAGMATISM IN TIN-BEARING AREAS OF EASTERN YAKUTIA
Authors
Vera Trunilina
Proceedings
SGEM International Multidisciplinary Scientific GeoConference EXPO Proceedings; 18th International Multidisciplinary Scientific GeoConference SGEM2018, Science and Technologies in Geology, Exploration and Mining
Publisher
STEF92 Technology
Year
2018
Pages
577-588
SWS Citekey
Trunilina20181577588
ISSN
1314-2704
ISBN
978-619-7408-35-5
Language
en
Publication type
Conference Paper
Keywords
granitoidsmantle magmatismsources of ore elements
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