Calcite and dolomite relations in Svecofennian carbonate rocks
作者:
Erik Högberg,
期刊:
Geologiska Föreningen i Stockholm Förhandlingar
(Taylor Available online 1962)
卷期:
Volume 84,
issue 3
页码: 283-310
ISSN:0016-786X
年代: 1962
DOI:10.1080/11035896209452952
出版商: Taylor & Francis Group
数据来源: Taylor
摘要:
In this paper, the author summarizes his investigations into the occurence and distribution of dolomite and magnesium-silicate minerals in Svecofennian carbonate rocks. As a result of his investigations, the author has come to the conclusion that it is very probable that dolomite rocks have originated in a prehistoric sea, either by direct chemical precipitation or dolomitization of limestone during an early stage of diagenesis. The theory that dolomitization first occurred during the orogenic period of the Svecofennian evolution, which theory is propounded in current Swedish literature, is considered unlikely. On the other hand the opposite is possible,i.e., that the dolomite rocks were partially de-dolomitized during a period of metamorphism and gave rise to limestone and solutions containing magnesium which could result in magnesia metasomatism of the contiguous rocks.
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