The process of regional-residual separation in potential field is age-old. Broadly, there are
two techniques for regional-residual resolution, viz., graphical and analytical. Both the …

Unconformity related uranium mineralisation occurs in Banganapalle Formation of Palnad
Sub-basin, Cuddapah Basin. Several evidences of hydrothermal activity exist in both …

Uranium exploration in the Cuddapah Basin is both scientifically and logistically
challenging. An integrated multidisciplinary approach is adopted to infer the subsurface …

The Mesoproterozoic Cuddapah Basin (CB), together with its inclusive Neoproterozoic
Kurnool Basin, constitutes India's second largest Proterozoic (Purana) basin. It has an areal …

Fracture and fault zones can tap the uranium-bearing fluid and help to migrate into the
structural trap where the hydrothermal fluids cool and precipitate the uranium mineral. Such …

The aim of the research is to delineate the host rock of uranium in the semi-arid regions of
Andhra Pradesh, India. Uranium is one of India's major rich resources explored in recent …

Middle Proterozoic Gulcheru Quartzite marks tlie onset of sedimentation, after the
Eparchaean unconforrnity, in the Cuddapah Basin. In the southwestern margin of the basin it …

Abstract The Vempalle Formation of the Proterozoic Cuddapah basin has a well developed
sequence of carbonate rocks, which are interbedded with shales, siltstones and chert. The …

The Bhima basin, the youngest (~ 0.625-0.55 Ga) and the smallest (~ 5,300 sq km in area)
amongst the intracratonic 'Purana basins'(Meso-/Neo-proterozoic) of India, has become the …

The X-ray diffraction (XRD) studies reveal that in syngenetically-mineralised (widespread)
Neoarchaean to Palaeoproterozoic basement granitoids, the primary uranium minerals …