The Rise of the Tibetan Plateau as a Consequence of Progressive Underthrusting of the Indian Lithosphere Driven by Subduction of the Giant India-Australia Plate at the Sumatra-Java Trench
The Rise of the Tibetan Plateau as a Consequence of Progressive Underthrusting of the Indian Lithosphere Driven by Subduction of the Giant India-Australia Plate at the Sumatra-Java Trench
