Peninsular India forms a keystone in Gondwana, linking the East African and Malagasy
orogens with Ediacaran–Cambrian orogenic belts in Sri Lanka and the Lützow Holm Bay …

Lying to the south of the Dharwar Craton, the expansive granulite massif, known as the
Granulite Terrane of South India, preserves protracted history of the earth from ca. 3400–500 …

Although many recent reviews emphasize a uniformity in granulite pressure–temperature (P–
T) conditions and paths, granulites in reality preserve a spectrum of important petrogenetic …

In general, Archean rocks exhibit rather ordinary moderate-P-high-T facies series
metamorphism; neither blueschists nor any record of deep continental subduction and return …

Southern India occupies a central position in the Late Neoproterozoic–Cambrian Gondwana
supercontinent assembly. The Proterozoic mosaic of southern India comprises a collage of …

This study assesses temperatures of formation of common granulites by combining
experimental constraints on the P–T stability of granulite-facies mineral associations with a …

There are three geothermometers based on reversed experimental data and applicable to
granulites: the two-pyroxene, two-oxide, and garnet-clinopyroxene thermometers. All have …

Nd-isotope analyses from a range of lithologies, including charnockites, metasediments, and
granitoids that comprise the high-grade terrain of South India define contrasting age …

Abstract The Mozambique Ocean closed as Gondwana formed. Its suture has been
identified in Madagascar (Betsimisaraka suture), but its continuation, into India, is …

Cratons and Fold Belts of India, is a unique attempt at presenting geological characteristics
and evolution of the fold belts and the cratonic areas of the Indian shield. The author has …