has been cited by the following article(s):
[1]
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Proterozoic Charnockites at 1.6 & 1.0 Ga in the Eastern Ghats Belt, India, Mirror Secular Evolution of Continental Crust
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2016 |
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[2]
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AN EXOTIC TERRANE AT THE WESTERN MARGIN OF THE EASTERN GHATS BELT, INDIA
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INTERNATIONAL JOURNAL OF ADVANCEMENT IN EARTH AND ENVIRONMENTAL SCIENCES,
2014 |
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[3]
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Charnockite Massifs: Key to Tectonic Evolution of the Eastern Ghats Belt, India, and Its Columbia Connection
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Advances in Natural Science,
2014 |
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[4]
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EARLY MESOPROTEROZOIC THERMAL EVENT IN THE EASTERN GHATS PROVINCE, INDIA: U-PB ISOTOPIC EVIDENCE FROM SUPRACRUSTAL ROCKS
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INTERNATIONAL JOURNAL OF ADVANCEMENT IN EARTH AND ENVIRONMENTAL SCIENCES,
2013 |
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[5]
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Vad kan inneslutningar i zirkon ber?tta om Varbergscharnockiten, SV Sverige
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NULL
2013 |
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[6]
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How long-lived is ultrahigh temperature (UHT) metamorphism? Constraints from zircon and monazite geochronology in the Eastern Gh
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Precambrian Research,
2013 |
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[7]
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Vad kan inneslutningar i zirkon berätta om Varbergscharnockiten, SV Sverige
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2013 |
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[8]
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The tectonic evolution of the Ongole Domain, India: A metamorphic and geochronological approach
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2011 |
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[1]
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Ubiquitous Chemical Signature in Khondalites of Eastern Ghats Granulite Belt, a Possible Explanation
Journal of the Geological Society of India,
2023
DOI:10.1007/s12594-023-2323-z
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[2]
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How long-lived is ultrahigh temperature (UHT) metamorphism? Constraints from zircon and monazite geochronology in the Eastern Ghats orogenic belt, India
Precambrian Research,
2013
DOI:10.1016/j.precamres.2012.12.001
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