Harmsarvet, a silver-rich ore in south central Sweden
作者:
Gunnar Eriksson,
Kees Kieft,
期刊:
Geologiska Föreningen i Stockholm Förhandlingar
(Taylor Available online 1980)
卷期:
Volume 102,
issue 2
页码: 57-65
ISSN:0016-786X
年代: 1980
DOI:10.1080/11035898009450876
出版商: Taylor & Francis Group
关键词: Mineral deposits;genesis;ore deposits;mineralisation;native silver;sulfides;argentite;acanthite;sulfosalts;sternbergite;sphalerite;pyrrhotite;chalcopyrite;cubanite;galena;fluorite;rare earths;minor elements;biotite gneiss;Precambrian;Harmsarvet;Falun;Dala
数据来源: Taylor
摘要:
The silver-rich zinc-lead sulfide deposit of Harmsarvet, 14 km NW of the famous ore deposits of Falun, south central Sweden, is located in a series of Precambrian biotite gneisses, about 2 km SE of a monzonite intrusion. Host rock to the mineralisation has undergone hydrothermal alteration, with especially sericitisation and saussuritisation on a large scale. The silver minerals are native silver, acanthite and silver-antimony-sulfosalts with an important part of the silver present as submicroscopic inclusions in secondary pyrite formed at the expense of pyrrhotite. On average, ore contains 0.39% Ag. A temperature of at least 177°C is proposed for the formation of the major part of the mineralisation.
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