Relief surveying and chronology study were carried out on the deformed river terraces across the Artushi anticline belt in the northwestern Tarim Basin. The crust shortening rate of this anticline belt since late Plei...Relief surveying and chronology study were carried out on the deformed river terraces across the Artushi anticline belt in the northwestern Tarim Basin. The crust shortening rate of this anticline belt since late Pleistocene was calculated to be up to 5-6 mm/a. The total crust shortening rate from the northwestern Tarim Basin to southwestern Tianshan since late Pleistocene was estimated to be over 10 mm/a.展开更多
People pay more and more attention to the coupling relation between ground and air.In seismogenic process, thermal anomaly and temperature redistribution are generated not onlyin source region but also in its surround...People pay more and more attention to the coupling relation between ground and air.In seismogenic process, thermal anomaly and temperature redistribution are generated not onlyin source region but also in its surrounding areas. This causes various thermal effects展开更多
基金This work was supported by the National Natural Science Foundation of China (Grant No. 49834005) the Commission of Science and Technology of China (Grant No. 96-913-07-01) and the Key Project of the Earthquake Joint Foundation (Grant No. 9507438).
文摘Relief surveying and chronology study were carried out on the deformed river terraces across the Artushi anticline belt in the northwestern Tarim Basin. The crust shortening rate of this anticline belt since late Pleistocene was calculated to be up to 5-6 mm/a. The total crust shortening rate from the northwestern Tarim Basin to southwestern Tianshan since late Pleistocene was estimated to be over 10 mm/a.
文摘People pay more and more attention to the coupling relation between ground and air.In seismogenic process, thermal anomaly and temperature redistribution are generated not onlyin source region but also in its surrounding areas. This causes various thermal effects
