Abstract The East African Orogen, extending from southern Israel, Sinai and Jordan in the
north to Mozambique and Madagascar in the south, is the world́s largest Neoproterozoic to …

Shear zones play a major role in the deformation of the crust at a variety of scales, as
expressions of strain localization during orogeny and rifting, and also as reactivated …

Available U–Pb geochronology of the Precambrian shield of Madagascar is summarized
and integrated into a synthesis of the region's geological history. The shield is described in …

Gondwana was consolidated in the late Cambrian after 180 myr of tectonic convergence
among Neoproterozoic paleocontinents and smaller fragments. We present a compilation of …

Abstract LA-ICP-MS U-Pb dates and EPMA trace-element maps of titanite were collected
from calc-silicate gneisses of the Ikalamavony (peak T: 750–800° C) and Anosyen (peak T …

We report the discovery of osumilite in ultrahigh‐temperature (UHT) metapelites of the
Anosyen domain, southern Madagascar. The gneisses equilibrated at~ 930° C/0.6 GPa …

Length scales of compositional heterogeneity in titanite from 750 to 1000° C metamorphic
rocks from southern Madagascar were measured to provide empirical constraints on …

Late tectonic, post-collisional granite suites are a feature of many parts of the Late
Neoproterozoic to Cambrian East African Orogen (EAO), where they are generally attributed …

Abstract The Neoproterozoic geology of East Africa records the events leading up to the
formation of Gondwana and subsequently Pangea, and hence understanding the …

This study provides further evidence for a Cryogenian (∼ 770–760 Ma) deformation event in
NW India, a region generally regarded tectonically stable during the Rodinia to Gondwana …