Peninsular India is a collage of Archaean cratonic domains separated by Proterozoic mobile belts. A number of cratonic basins, known as “Purana basins” in the Indian literature, formed …
The sedimentary sequences and associated magmatic rocks from the Cuddapah basin and adjoining fold belts on the eastern margin of the Dharwar craton of Peninsular India are …
In this study, textural relations coupled with mineral chemistry of hydrothermal magnetite, fluorapatite, monazite and allanite from the Mohuldih uranium deposit in the Singhbhum …
Significance of Precambrian and early Cambrian palaeobiological remains recorded over the last few years on the Indian subcontinent are discussed in the present review. The …
We propose a Precambrian megacraton (consisting of two or more ancient cratons), DHABASI in the Indian Shield, which includes the Dharwar, Bastar and Singhbhum cratons …
Two distinct NW-to WNW-trending mafic dike swarms of the previously dated ca. 2.21 Ga Anantapur-Kunigal and ca. 2.18 Ga Mahbubnagar-Dandeli swarms, emplaced in the …
T Deb, J Mallik - Journal of Earth System Science, 2022 - Springer
A complex magma mingling/interaction zone in the Bundelkhand craton, Central India, was formed when several pulses of mafic magma interacted with the still-crystallising felsic …
The Cuddapah basin in southern India is one of the large Proterozoic basins with rich and strategic mineral resources. As a repository of sedimentary and tectonic records spanning …
FC Junior, F Guadagnin - Chemostratigraphy Across Major …, 2018 - Wiley Online Library
The Paleoproterozoic era was an interval of major changes in Earth, whereas the Mesoproterozoic era comprised the “boring billion” due to the paucity of changes, especially …