1·The paper also discusses the structural evolution history of the foreland basin in Mesozoic.
并讨论了龙门山中段中生代前陆盆地的构造演化历史。
2·Zengmu basin is a peripheral foreland basin, formed from southern subduction of Nansha Block and gentle collision with Borneo Block, and experienced four stages of tectonic evolution.
曾母盆地是南沙块体向南俯冲与婆罗洲块体发生软碰撞而形成的一个周缘前陆盆地，经历了四个不同的构造演化阶段。
3·The late Permian it was changed into the back arc basin, and transformed into foreland basin.
晚二叠世末，该地区变成弧后盆地，进一步转化成前陆盆地。
4·With the uplift of marginal mountains, three foreland basin systems were formed in Juggar basin.
随着周缘界山的隆升，准噶尔盆地形成三大前陆盆地系统。
5·The lithological feature of the sediments in the foreland basin reflects the double-source supply and the orogenic-belt erosion.
前陆盆地沉积物的岩石学特征反映了双物源供给和造山带的剥蚀。