Ordos block was squeezed by the Qinghai-Tibetan block and North China block,and the tectonic activity was intense. In the periphery of Ordos block,there was a series of folds zones and compressed faults with complicat...Ordos block was squeezed by the Qinghai-Tibetan block and North China block,and the tectonic activity was intense. In the periphery of Ordos block,there was a series of folds zones and compressed faults with complicate structures. This paper used three-phase data of 1980,1990 and 2014 to calculate vertical velocity of Northwestern margin of Ordos and the analytical results indicated that(1) the Hetao basin between the rise of Yinshan fault block and Ordos fault block showed relatively subsidence,in which Linhe basin was the most evident and the subsidence rate was about 2-4 mm/a. The subsidence rate of Jartai-Yinchuan rift zone on the western margin of Ordos block was about 2 mm/a;(2) the whole testing zone exhibited the evident inherited movement characterized by mountain rise and basin subsidence;(3) the two leveling section through the northern margin fault and Dengkou-Benjing fault showed that the difference between vertical velocities on two sides of the fault was less than 0. 5 mm/a.展开更多
基金funded by the Director Fund of the First Monitoring and Application Center,China Earthquake Administration(FMC2014001)the North China Project of Integrated Geophysical Field Observations of China(201508009)
文摘Ordos block was squeezed by the Qinghai-Tibetan block and North China block,and the tectonic activity was intense. In the periphery of Ordos block,there was a series of folds zones and compressed faults with complicate structures. This paper used three-phase data of 1980,1990 and 2014 to calculate vertical velocity of Northwestern margin of Ordos and the analytical results indicated that(1) the Hetao basin between the rise of Yinshan fault block and Ordos fault block showed relatively subsidence,in which Linhe basin was the most evident and the subsidence rate was about 2-4 mm/a. The subsidence rate of Jartai-Yinchuan rift zone on the western margin of Ordos block was about 2 mm/a;(2) the whole testing zone exhibited the evident inherited movement characterized by mountain rise and basin subsidence;(3) the two leveling section through the northern margin fault and Dengkou-Benjing fault showed that the difference between vertical velocities on two sides of the fault was less than 0. 5 mm/a.
