Brittle tectonothermal evolution in the Forsmark area, central Fennoscandian Shield, recorded by paragenesis, orientation and 40Ar/39Ar geochronology of fracture minerals

Author:

Sandström Björn,Tullborg Eva-Lena,Larson Sven Åke,Page Laurence

Funder

Svensk Kärnbränslehantering

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference101 articles.

1. The Gothian and Labradorian orogens: variations in accretionary tectonism along a late Paleoproterozoic Laurentia–Baltica margin;Åhäll;GFF,1997

2. Sm–Nd isotope determination of low-temperature fluorite–calcite–galena mineralization in the margins of the Fennoscandian Shield;Alm,2005

3. Metamorphic and basin fluids in quartz–carbonate–sulphide veins in the SW Scottish Highlands: a stable isotope and fluid inclusion study;Anderson;Geofluids,2004

4. The Scandinavian Alum Shales;Andersson,1985

5. Petrogenesis of Mesoproterozoic (Subjotnian) rapakivi complexes of central Sweden; implications from U–Pb zircon ages, Nd, Sr and Pb isotopes;Andersson;Transactions of the Royal Society of Edinburgh: Earth Sciences,2002

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