Time constraints on the deposition of a mineralisation-proximal metavolcaniclastic rock at Byngsbodberget, northwest of Falun, Bergslagen, Sweden

IF 1.2 4区 地球科学 Q2 GEOLOGY Gff Pub Date : 2021-05-04 DOI:10.1080/11035897.2021.1896573
Alexander Lewerentz, M. Ripa, G. Morris
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引用次数: 1

Abstract

ABSTRACT Metavolcanic rocks in the area north and northwest of Falun, Bergslagen, Sweden host numerous mineralisations and historic mines. The stratigraphy and formation ages of these metavolcanic rocks however remains unresolved on the local scale. This study aims to add at least some pieces to that puzzle by exploring age-constrains for the deposition of a metavolcaniclastic rock at Byngsbodberget, c. 15 km west-northwest of Falun. U-Pb SIMS analyses were conducted on zircon, from which a concordia age is calculated at 1900 ± 9 Ma and interpreted as the age of the main volcanic event that contributed material to the studied volcaniclastic rock. Based on observations of way-up indicators, this is thought to mark the lower parts of the local volcanic stratigraphy.
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瑞典贝格斯拉根法轮西北部Byngsbodberget矿化近端变质火山碎屑岩沉积的时间限制
瑞典贝格斯拉根法轮北部和西北部地区的变质火山岩中有许多矿化和历史悠久的矿山。然而,这些变质火山岩的地层和形成年龄在局部尺度上仍未得到解决。这项研究的目的是通过探索位于法轮西北偏西15公里处的Byngsbodberget的一处变火山碎屑岩沉积的年龄限制,至少为这个谜团增加一些线索。对锆石进行了U-Pb SIMS分析,计算出concordia年龄为1900±9 Ma,并将其解释为主要火山事件的年龄,该火山事件为所研究的火山碎屑岩提供了物质。根据对向上指示的观察,这被认为标志着当地火山地层的下部。
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来源期刊
Gff
Gff 地学-地质学
CiteScore
2.80
自引率
10.00%
发文量
11
审稿时长
>12 weeks
期刊介绍: GFF is the journal of the Geological Society of Sweden. It is an international scientific journal that publishes papers in English covering the whole field of geology and palaeontology, i.e. petrology, mineralogy, stratigraphy, systematic palaeontology, palaeogeography, historical geology and Quaternary geology. Systematic descriptions of fossils, minerals and rocks are an important part of GFF''s publishing record. Papers on regional or local geology should deal with Balto-Scandian or Northern European geology, or with geologically related areas. Papers on geophysics, geochemistry, biogeochemistry, climatology and hydrology should have a geological context. Descriptions of new methods (analytical, instrumental or numerical), should be relevant to the broad scope of the journal. Review articles are welcome, and may be solicited occasionally. Thematic issues are also possible.
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