%e0%a6%9c%e0%a6%be%e0%a6%a8%e0%a7%8d%e0%a6%a8%e0%a6%be%e0%a6%a4 %e0%a6%a4%e0%a7%8b%e0%a6%b9%e0%a6%be %e0%a6%ad%e0%a6%be%e0%a6%87%e0%a6%b0%e0%a6%be%e0%a6%b2 %e0%a6%b2%e0%a6%bf%e0%a6%82%e0%a6%95 %e0%a6%9f%e0%a7%87%e0%a6%b2%e0%a6%bf%e0%a6%97%e0%a7%8d%e0%a6%b0%e0%a6%be%e0%a6%ae [Top-Rated]
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 Western Ghats region is a part of the larger Indian Shield, a geological province that encompasses much of southern India. The region has undergone multiple phases of tectonic activity, including rifting, collision, and volcanism, which have contributed to its complex geological history. The charnockite and Bharivar lava sequences are products of these tectonic processes and offer valuable clues about the region's evolution. The region has undergone multiple phases of tectonic
The field relationships between the charnockites and Bharivar lava flows provide important insights into their temporal and spatial relationships. The charnockites are often found as xenoliths within the Bharivar lavas, indicating that the lavas post-date the charnockites. The charnockites are often found as xenoliths within
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 Western Ghats region is a part of the larger Indian Shield, a geological province that encompasses much of southern India. The region has undergone multiple phases of tectonic activity, including rifting, collision, and volcanism, which have contributed to its complex geological history. The charnockite and Bharivar lava sequences are products of these tectonic processes and offer valuable clues about the region's evolution.
The field relationships between the charnockites and Bharivar lava flows provide important insights into their temporal and spatial relationships. The charnockites are often found as xenoliths within the Bharivar lavas, indicating that the lavas post-date the charnockites.