Continental crustal growth rates, crustal volumes/thicknesses, and continental freeboard are
considered to be intimately related; however none are easy to quantify, least of all in the …

The Palaeoproterozoic–Mesoproterozoic transition (∼ 1600 Ma) is a significant event in the
Earth history as a global thermal perturbation affected the pre-1600 Ma landmasses. Like …

The Proterozoic volcano-sedimentary succession comprising successively younger
Dhanjori, Chaibasa, Dhalbhum, Dalma and Chandil Formations of the Singhbhum crustal …

Abstract The Mesoarchaean–Palaeoproterozoic stratigraphic record of the Singhbhum
crustal province, eastern India, implies sedimentation and volcanism in a changing tectonic …

The 2.7–2.0 Ga volcano-sedimentary records of the African, Indian and Australian cratons
indicate two broadly defined periods of extensive drowning of the emergent continental …

An integrated chronicle of major events leading to the growth of the pre-2.0 Ga Indian
Craton, which is the aim of this paper, is an essential requirement to constrain the possibility …

The Kolhan Group in the Singhbhum Craton of eastern India is a passive margin siliciclastic
shelf to deep‐water carbonate ramp platform succession. It occupies a unique position in …

Abstract The Singhbhum Craton has a limited Palaeoproterozoic supracrustal record, which
suggests a three-part history, comprising: a long period of high freeboard and palaeosol …

Abstract The Paleoproterozoic-Mesoproterozoic boundary is associated with onset of
supercontinental cycle and global thermal perturbation. In the Singhbhum cratonic province …

Abstract The Paleo-Mesoproterozoic North Singhbhum Mobile Belt (NSMB) is a fold-thrust
belt typically found in a collisional setting and is well known for hosting gold mineralisation …