Distribution of K, Rb, Sr and Ba in Nain anorthosite plagioclase

Details Distribution of K, Rb, Sr and Ba in Nain anorthosite plagioclase Distribution of K, Rb, Sr and Ba in Nain anorthosite plagioclase

Mar 1970

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1970gecoa..34..401g&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 34, Issue 3, pp.401-408

Mathematics

Logic

3

Scientific paper

Plagioclases from a Labrador anorthosite have ratios >1000 but this does not delimit a possible parental material. Other trace element ratios support (1960) geological subdivision of the anorthosite. Poor correlation between ratios and per cent K may result from varying amounts of phases co-existing with plagioclase, loss of exsolved K-feldspar, or regionally prevailing P-T conditions.

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