The repeatedly gravimetric data in western area of Yunnan Province are analyzed. The dynamic evolution characteristics of gravity field in the seismogenic process of the Panzhihua Ms6.1 earthquake on Aug. 30,2008 in Sichuan Province and Yaoan Ms6.0 on Jul. 9,2009 in Yunnan Province are studied and the following conclusions are drawn. 1)The gravity observations reflected the precursory gravity information during the seismogenic process, the dynamic evolution pattern of gravity reflects clearly the gravity field’s evolution of “quasihomogeneous→heterogeneous then earthquake→quasihomogeneous” in the process of the Pabzhihua Ms6.1 and Yaoan Ms6.0 earthquakes.2)The tendency after Panzhihua Ms6.1 earthquake are estimated and the annual prediction before Yaoan Ms6.0 earthquake are made.
The crust of the Tibetan plateau and its adjacent area is divided into two layers: the elastic brittle layer and the viscoelastic ductile layer, and then the interior temperature field of the crust by steady heat conductive equation is evaluated.Further, under the condition that fracture intensity is equal to creeping intensity, brittleductile transition plane is obtained by use of Crust2.0 earth model. The results show that brittleductile transition plane locates in middle crust about 20-35 km depth generally. The thicker the crust is, the deeper the transition floor is. Effective viscosity of transition plane located in Tibetan plateau is between
10 19-10 22 Pas, temperature field is between 450-600℃.