The stratigraphic position of the intrusive rocks of Umeå, northern Sweden
作者:
Karel Miškovský,
期刊:
Geologiska Föreningen i Stockholm Förhandlingar
(Taylor Available online 1984)
卷期:
Volume 106,
issue 1
页码: 59-66
ISSN:0016-786X
年代: 1984
DOI:10.1080/11035898409454608
出版商: Taylor & Francis Group
关键词: Svecokarelian rocks;Hänö series;Umeå intrusives;primorogenic intrusives;Västerbotten county;northern Sweden;N6340 N6355 E2010 E2025
数据来源: Taylor
摘要:
The Svecokarelian supracrustal and infracrustal rocks of the Umeå district have been studied within an area of about 350 km2. Intrusive rocks constitute ca. 5% of the research area, a considerably lower proportion than in other parts of the Våsterbotten county. The intrusives of Umeå are now mostly gneissose and conforming to the surrounding metasediments. High metamorphism and locally moderate veining and/or migmatization are normal features of the intrusive rocks. The range of mineralogical and chemical composition is from gabbro to tonalite and a low Al-value points to I-type granitoids. These rocks may be more comparable with the primorogenic-synorogenic intrusives of the Jörn suite than, as suggested earlier, with those of the Revsund granite.
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