Rubidium-strontium isochron ages of the crystalline core of the Tatra mountains, Poland

1 December 1968

journal article
Published by American Journal of Science (AJS) in American Journal of Science

Vol. 266 (10) , 895-907
https://doi.org/10.2475/ajs.266.10.895

Abstract

Absolute age of main quartz diorite massif of 290-300 m.y., whole rock isochron age of 420 m.y., absence of metamorphic recrystallization during late Cretaceous orogeny

Keywords

QUARTZ
RECRYSTALLIZATION
ISOCHRON AGES
RUBIDIUM STRONTIUM
STRONTIUM ISOCHRON
CRYSTALLINE CORE
M.Y

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