Cenozoic volcanism has been well studied in northern, eastern and southwestern Tibet (Coulon et al., 1986; Arnund et al., 1992; Turner et al., 1993, 1996; Deng, 1978, 1998; Miller et al., 1999, Wang e
Determining the timing, magnitude, and location of deformation due to the Indo|Asian collision is widely acknowledged as an important step in understanding how the lithosphere responds during contine