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Publikováno v:
The Deep Proterozoic Crust in the North Atlantic Provinces ISBN: 9789401089074
The high-grade low-pressure metamorphism in Rogaland increases towards the southwest to reach a maximum near the border of the Egersund intrusive complex. The first isograd is the “hypersthene line”, marking the appearance of hypersthene in rocks
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2abc4982ed42a00102367fe812e0a268
https://doi.org/10.1007/978-94-009-5450-2_28
https://doi.org/10.1007/978-94-009-5450-2_28