摘要
<正>1.Introduction Intra-continental deformation and metamorphism are related to crustal thickening,crustal thinning,exhumation of highgrade metamorphic rocks,and basin formation during the terminal stages of continental collision(Davis et al.,1986;Mc Donough and Simony,1988;Yin,2004;Lee et al.,2004;Faure et al.,2005).
引文
1)Burchfiel,B.C.,Wang,E.Q.,2003.Northwest-trending,middle Cenozoic,left-lateral faults in southern Yunnan,China,and their tectonic significance.Journal of Structural Geology,25,718-792.
2)Wang G.,Wan J.L.,Wang E.Q.,Zheng,D.W.,Li,F.,2008.Late Cenozoic to recent transtensional deformation across the Southern part of the Gaoligong shear zone between the Indian plate and SE margin of the Tibetan plateau and its tectonic origin.Tectonophysics,460,1-20.
3)Xu,Z.Q.,Wang,Q.,Cai,Z.H.,Dong,H.W.,Li,H.Q.,Chen,X.J.,Duan,X.D.,Cao,H.,Li,J.,Burg,J-P.,2015.Kinematics of the Tengchong Terrane in SE Tibet from the late Eocene to early Miocene:Insights from coeval mid-crustal detachments and strike-slip shear zones.Tectonophysics.665,127-148.