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Geochronological studies have provided a temporal framework for understanding the evolution of these rocks. The charnockites of the Western Ghats have been dated to around 2.5-2.7 Ga, while the Bharivar lava flows are believed to have erupted at around 2.2-2.3 Ga.

The charnockite to Bharivar lava sequences in the Western Ghats region represent a fascinating chapter in the geological history of Western India. These rocks offer a glimpse into the complex processes that have shaped the region, including high-pressure metamorphism, volcanic activity, and tectonic interaction. Further research on these rocks will continue to provide valuable insights into the evolution of the Indian Shield and the geological history of the Western Ghats. These rocks offer a glimpse into the complex

The charnockites of the Western Ghats are thought to have formed through the metamorphism of basic and ultrabasic rocks under high-pressure and high-temperature conditions. This process involved the interaction of crustal and mantle rocks, leading to the formation of a distinctive mineral assemblage. This process involved the interaction of crustal and

The Western Ghats, a mountain range that runs along the western coast of India, is one of the most significant geological features of the region. This mountain range is composed of a variety of rock types, including charnockites, which are a type of metamorphic rock. Charnockites are characterized by their unique mineral composition, primarily consisting of quartz, feldspar, and pyroxene. These rocks are formed through the metamorphism of basic and ultrabasic rocks under high-pressure and high-temperature conditions. primarily consisting of quartz