Abstract
The paper presents geochronological data on silicate and endogenic carbonate rocks from the Oshurkovo apatite-bearing pluton, namely, the U-Pb and Rb-Sr isochron ages of gabbros and carbonatites.
The U-Pb age of the carbonatites from this pluton (126.55 ± 0.85 Ma) is close to that of the other carbonatite occurrences in southwestern Transbaikalia. Also, its similarity to the age of the gabbro (125.4 ± 2 Ma), which makes up the bulk of the pluton, suggests that these rocks are comagmatic.
You do not have access to this content, please speak to your institutional administrator if you feel you should have access.