His scientific interests lie mostly in Zircon, Geochemistry, Petrology, Paleontology and Geochronology. His research in Zircon intersects with topics in Basement, Gneiss and Pluton. Manoj K. Pandit studies Archean, a branch of Geochemistry.
His study in Mafic and Felsic is carried out as part of his Petrology studies. Rodinia, Craton, Precambrian, Gondwana and Paleomagnetism are the core of his Paleontology study. The various areas that Manoj K. Pandit examines in his Craton study include Proterozoic and Ultramafic rock.
Manoj K. Pandit mainly investigates Geochemistry, Paleontology, Petrology, Proterozoic and Craton. His work in Geochemistry covers topics such as Fold which are related to areas like Rift and Shear zone. Paleomagnetism, Gondwana, Rodinia, Precambrian and Supercontinent are among the areas of Paleontology where the researcher is concentrating his efforts.
His work in Rodinia addresses subjects such as Sedimentary rock, which are connected to disciplines such as Sedimentary depositional environment. Crust is closely connected to Magmatism in his research, which is encompassed under the umbrella topic of Petrology. His Proterozoic research focuses on Granulite and how it relates to Mantle and Carbonatite.
Manoj K. Pandit spends much of his time researching Geochemistry, Craton, Paleontology, Archean and Supercontinent. As part of his studies on Geochemistry, Manoj K. Pandit often connects relevant areas like Large igneous province. Manoj K. Pandit has researched Craton in several fields, including Paleomagnetism, Hadean, Crust and Geochronology.
Within one scientific family, Manoj K. Pandit focuses on topics pertaining to Tectonics under Archean, and may sometimes address concerns connected to Feldspar. His Supercontinent research is multidisciplinary, incorporating perspectives in Rodinia and Continental crust. His Rodinia research incorporates elements of Gondwana and Mantle.
His primary scientific interests are in Geochemistry, Mafic, Zircon, Archean and Supercontinent. Manoj K. Pandit is interested in Igneous rock, which is a field of Geochemistry. Manoj K. Pandit has included themes like Felsic and Volcanic rock in his Igneous rock study.
His studies in Mafic integrate themes in fields like Petrogenesis, Dharwar Craton, Granulite, Gondwana and Terrane. The Archean study combines topics in areas such as Paleomagnetism, Craton and Crust. Manoj K. Pandit interconnects Rodinia, Magmatism and Continental crust in the investigation of issues within Supercontinent.
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Precambrian crustal evolution of Peninsular India: A 3.0 billion year odyssey
Joseph G. Meert;Manoj K. Pandit;Vimal R. Pradhan;Jonathan Banks.
Journal of Asian Earth Sciences (2010)
Paleomagnetism and Detrital Zircon Geochronology of the Upper Vindhyan Sequence, Son Valley and Rajasthan, India: A ca. 1000 Ma Closure age for the Purana Basins?
S.J. Malone;J.G. Meert;D.M. Banerjee;M.K. Pandit.
Precambrian Research (2008)
Paleomagnetism and geochronology of the Malani Igneous Suite, Northwest India: Implications for the configuration of Rodinia and the assembly of Gondwana
Laura C. Gregory;Joseph G. Meert;Bernard Bingen;Manoj K. Pandit.
Precambrian Research (2009)
The Proterozoic magmatic and metamorphic history of the Banded Gneiss Complex, central Rajasthan, India: LA-ICP-MS U–Pb zircon constraints
Ian Buick;Charlotte M Allen;M Pandit;Daniela Rubatto.
Precambrian Research (2006)
A paleomagnetic and geochronologic study of the Majhgawan kimberlite, India: Implications for the age of the Upper Vindhyan Supergroup
Laura C. Gregory;Joseph G. Meert;Vimal Pradhan;Vimal Pradhan;Manoj K. Pandit.
Precambrian Research (2006)
Paleomagnetic and geochronological studies of the mafic dyke swarms of Bundelkhand craton, central India: Implications for the tectonic evolution and paleogeographic reconstructions
Vimal R. Pradhan;Joseph G. Meert;Manoj K. Pandit;George Kamenov.
Precambrian Research (2012)
Age, petrogenesis and significance of 1 Ga granitoids and related rocks from the Sendra area, Aravalli Craton, NW India
M.K. Pandit;L.M. Carter;L.D. Ashwal;R.D. Tucker.
Journal of Asian Earth Sciences (2003)
Constraints on the Proterozoic evolution of the Aravalli-Delhi Orogenic belt (NW India) from monazite geochronology and mineral trace element geochemistry
Ian Buick;C Clark;Daniela Rubatto;Joerg Hermann.
Lithos (2010)
Late Paleoproterozoic magmatism in Delhi Fold Belt, NW India and its implication: evidence from EPMA chemical ages of zircons
S. Biju-Sekhar;K. Yokoyama;M.K. Pandit;T. Okudaira.
Journal of Asian Earth Sciences (2003)
India's changing place in global Proterozoic reconstructions: A review of geochronologic constraints and paleomagnetic poles from the Dharwar, Bundelkhand and Marwar cratons
Vimal R. Pradhan;Joseph G. Meert;Manoj K. Pandit;George Kamenov.
Journal of Geodynamics (2010)
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