Geochemistry of high grade metamorphic rocks, Lofoten-Vesterålen North Norway

Details Geochemistry of high grade metamorphic rocks, Lofoten-Vesterålen North Norway Geochemistry of high grade metamorphic rocks, Lofoten-Vesterålen North Norway

Jan 1971

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1971gecoa..35...89h&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 35, Issue 1, pp.89-99

Computer Science

25

Scientific paper

Ninety-one samples of granulite and amphibolite facies rocks were analysed for major elements and the trace elements Rb, Sr, Ba, Zr, Pb, Th and U. Rock units in amphibolite and granulite facies with comparable range in major element chemistries are significantly different in trace element contents. The granulite facies rocks are characterized by low Rb, Th and U concentrations. Their Pb concentrations are also significantly lower than in comparable amphibolite facies rocks. Subsequent, retrograde metamorphism does not noticeably affect the trace element concentrations of the rocks.

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