In this contribution, is presented evidence for ductile E-W extension in the Kung Co area of southern Tibet that took place at ~19 Ma and is associated with a major N-S trending normal fault.

This paper presents the results of new detailed geologic mapping, structural, kinematic, and quantitative thermobarometric investigations in Mabja Dome, southern Tibet, an area that has not been previously studied in such detail.

In this paper structural, thermobarometric and thermochronologic investigations of the Kangmar Dome, southern Tibet, suggest that both extensional and contractional deformational histories are preserved within the dome.