The Singhbhum craton of eastern India contains an almost continuous depositional record
from the Paleoarchean to the Neoproterozoic. Although researchers have examined the …

Spatially distributed, numerous conglomeratic units and coarser to finer clastic sedimentary
rocks which collectively constitute part of the Bisrampur Formation unconformably overlie the …

The Singhbhum craton of eastern India preserves an extensive record of basin formation
spanning the Paleoarchean to Neoarchean. Although spatially extensive and well exposed …

The stratigraphy of the Dhanjori basin placed at the northeastern margin of the Paleo-
Mesoarchean Singhbhum Craton has been revised. A mainly quartz-pebble conglomerate …

New U–Pb age and Hf isotope data obtained on detrital zircon grains from Au-and U-
bearing Archaean quartz-pebble conglomerates in the Singhbhum Craton, eastern India …

Distinguishing shallow-marine and terrestrial (fluvial) sedimentary deposits is often difficult
in the absence of fossils and challenging in deformed and metamorphosed early …

Studies on a wide range of gold deposit types suggest that the crustal accumulation of gold
throughout the Earth's history was a consequence of changing tectonic regimes and variable …

Abstract The arenite-dominant Mesoarchean Keonjhar Quartzite (> 700 m) succession
unconformably overlies the granitoid-greenstone core of the Singhbhum craton in the north …

Cratonic stabilization was a critical crustal process during the Hadean to Archean for the
formation of cratons. The understanding of how and where this process took place is …

Subaerial rise of Earth's first continents took place 3.3–3.2 Ga years ago. This had significant
influence on the ocean, atmosphere, and biosphere. Two important sedimentological …