An Integrated Magnetic Approach to Solving the Greater India Problem

Explore a comprehensive conference talk on the Greater India problem and its paleomagnetic implications. Delve into the complexities of determining the original surface area of Greater India, a crucial factor in understanding the India-Asia collision and its impact on Earth's tectonic history. Learn about the ongoing controversies surrounding the size of the Indian plate in Gondwanaland and the tectonic evolution of India, including its collision with Asia and the formation of the Tibetan Plateau. Discover how paleomagnetism and rock magnetism play pivotal roles in addressing these geological puzzles. Gain insights into innovative approaches for solving this paleomagnetic conundrum and enhancing our understanding of one of the most significant tectonic events in the Cenozoic era.