周缘前陆盆地 meaning in Chinese
peripheral foreland basin
pfb
Examples
- In the link party of qinling - qiliang - kunlun belt , the polyarc - basin systemic characteristic is discussed with strengthen and standout study on the detail relationship analysis between the arc - basin . the bayan har basin thought to be the preexistence of the songpan - garze belt , is a back - arc basin among a series of polyarc - basin systems behind the qiangtang - taniantawong front the arc beginning in the late paleozoic . the eastern margin started as the western passive continental margin of the yangtze block ( d - t2 ) , then changed into a foreland basin related to the north china block and the qiangtang block during the middle to late triassic
在秦祁昆仑结合部研究中，加强和突出了精细的岛弧盆分析和造山作用关系的研究，探讨了秦、祁、昆结合部多岛弧盆特征；通过巴颜喀拉地区沉积特征，沉积体的空间展布和形态，面式物源供给方式，矿物成分和地球化学背景分析，其沉积盆地属性总体上反映出一个从过渡地壳-洋壳基础上发育起来的周缘前陆盆地的发展和演化过程。 - By the integrated research on sedimentary - tectonic evolution and reformation of yanqi basin and the comparison of die evolution of northern tarim basin and tianshan belt , the result shows that yanqi basin experiences five evolution stages include forland basin ( t2 - 3 ) , extensional basin ( j ) , compression and denudation stage ( k ) , regional depression stage ( e ) , and broken intracontinental forland basin ( n + q ) . at mesozoic , kuche basin and yanqi basin belonged to a unity
对焉耆盆地沉积-构造演化及改造综合研究，并与塔里木盆地北部及天山构造带演化对比表明，今焉耆盆地先后经历了周缘前陆盆地( t2 - 3 ) 、伸展盆地( j ) 、挤压剥蚀阶段( k ) 、区域沉降( e )和破裂陆内前陆盆地( n + q )五大演化阶段。