In the framework of the Russian-Indian joint research projects geochemical and geochronological study of granitoid rocks across the Central Indian Tectonic Zone has been carried out. Geochronological data suggest that the Central Indian Tectonic Zone is composed primarily of Proterozoic rocks, formed as a result of several stages of granitoid magmatism: at 2.43, 2.34-2.31, 1.73-1.72 and 1.53-1.51 Ga. Metamorphic transformations reflected by Sm–Nd and Rb–Sr systems of rocks and minerals occurred 1.37-1.1 Ga ago that allows comparing the final processes in the Central Indian Tectonic Zone with the Grenville orogeny and it can be used for the reconstruction of Rodini
Many granitic bodies intrude the basement gneisses in Meghalaya Plateau, Northeast India. Rb-Sr whol...
Many granitic bodies intrude the basement gneisses in Meghalaya Plateau, Northeast India. Rb-Sr whol...
International audienceThe Godhra-Chhota Udepur (GC) sector (west-central India) is the zone of conve...
This item is only available electronically.The central Eastern Ghats Province is part of a series of...
The Late Archean-Early Proterozoic Mahakoshal greenstone belt (MGB) in central India is a 500 km lon...
The Kodaikanal–Palani Massif is an important component of India’sSouthern Granulite Terrain; underst...
The Sausar Mobile Belt at the southern margin of the Central Indian Tectonic Zone (CITZ) is a key un...
The Banded Gneiss Complex (BGC) of Rajasthan (NW India) is generally thought to be an Archaean basem...
The amphibolite facies Moyar, Bhavani and Palghat shear zones separate the South Indian Dharwar Crat...
The Banded Gneiss Complex (BGC) of Rajasthan (NW India) is generally thought to be an Archaean basem...
<div><p>The northern part of the central India tectonic zone (CITZ) is occupied by the Proterozoic M...
This paper reviews the state of structural and geochronological knowledge of Precambrian cratonic ro...
Granulites including a charnockite suite, mafic granulites, pelitic granulites, metanorite dykes and...
In this investigation, we reconstruct the latest Palaeoproterozoic to Early Mesoproterozoic orogenic...
The Sonapahar area of Shillong Meghalaya Gneissic Complex (SMGC) is an extension of the Central Indi...
Many granitic bodies intrude the basement gneisses in Meghalaya Plateau, Northeast India. Rb-Sr whol...
Many granitic bodies intrude the basement gneisses in Meghalaya Plateau, Northeast India. Rb-Sr whol...
International audienceThe Godhra-Chhota Udepur (GC) sector (west-central India) is the zone of conve...
This item is only available electronically.The central Eastern Ghats Province is part of a series of...
The Late Archean-Early Proterozoic Mahakoshal greenstone belt (MGB) in central India is a 500 km lon...
The Kodaikanal–Palani Massif is an important component of India’sSouthern Granulite Terrain; underst...
The Sausar Mobile Belt at the southern margin of the Central Indian Tectonic Zone (CITZ) is a key un...
The Banded Gneiss Complex (BGC) of Rajasthan (NW India) is generally thought to be an Archaean basem...
The amphibolite facies Moyar, Bhavani and Palghat shear zones separate the South Indian Dharwar Crat...
The Banded Gneiss Complex (BGC) of Rajasthan (NW India) is generally thought to be an Archaean basem...
<div><p>The northern part of the central India tectonic zone (CITZ) is occupied by the Proterozoic M...
This paper reviews the state of structural and geochronological knowledge of Precambrian cratonic ro...
Granulites including a charnockite suite, mafic granulites, pelitic granulites, metanorite dykes and...
In this investigation, we reconstruct the latest Palaeoproterozoic to Early Mesoproterozoic orogenic...
The Sonapahar area of Shillong Meghalaya Gneissic Complex (SMGC) is an extension of the Central Indi...
Many granitic bodies intrude the basement gneisses in Meghalaya Plateau, Northeast India. Rb-Sr whol...
Many granitic bodies intrude the basement gneisses in Meghalaya Plateau, Northeast India. Rb-Sr whol...
International audienceThe Godhra-Chhota Udepur (GC) sector (west-central India) is the zone of conve...