New whole-rock rare earth element (REE) data for the metacarbonate roc
ks interbedded with schists at Vinjamur in the Nellore Schist Belt of
Andhra Pradesh, show low total REE contents (Sigma 9-128 ppm) that are
inconsistent with an igneous carbonatitic origin but which correspond
more closely with a sedimentary limestone origin. The REE data of the
se rocks however, do not give absolute discrimination between marbles
of meta-limestone and metacarbonatite origin. Micro-probe analytical d
ata give better discrimination, and the chemical compositions of the c
alcite, micas, amphibole, plagioclase, apatite, monazite and staurolit
e in the Vinjamur marbles give strong and consistent evidence of a met
amorphosed sedimentary rather than an igneous origin.