By A Mystery Man Writer
Sweden is part of the Fennoscandian Shield, an area of old crystalline and metamorphic rocks, consolidated during hundreds of millions of years. Common rocks are gneiss, granite, granodiorite, sandstone and marble. The overburden is mainly formed by numerous periods of glaciation and deglaciation. The most common soil type is till, covering about 75 % of the landscape.
Isotope values of the bioavailable strontium in inland
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