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- Western Taiwan Foreland Basin 周缘前陆盆地
- Lasting, active tectonics accompanied with sediment supply from Taiwan orogen, results in modern West Taiwan Foreland Basin System. 持续的构造活动及伴随著造山带沈积物供应，形成今日的台湾西部前陆盆地系统。
- Chou, S.-C. Teng, Louis S. Chung, H.-S. and Shiao, T.-W. (1994) Geohistory analysis of west Taiwan foreland basin: a preliminary study. Petroleum Geology of Taiwan, 29, 289-323. 周素卿、邓属予、钟火盛、萧从文(1994)台湾西部前陆盆地地史分析初探。台湾石油地质，第29号，第289-323页。
- By employing sedimentary facies analysis on 3 outcrop sections and well-log stratigraphic studies the depositional systems and early development of the central Taiwan foreland basin have been established. 中文摘要台湾中部的桂竹林层沉积年代为晚中新世至早上新世，为台湾前陆盆地最老的地层，本层记录了由被动大陆边缘转变为前陆盆地的过程。
- Is Jurassic Chaidamu Basin a Foreland Basin? 柴达木侏罗纪盆地是"前陆盆地"吗?
- Age of Sichuan foreland basin is given. 确定了四川前陆盆地的形成时间。
- The Upper Triassic in the western Sichuan foreland basin can be divided into 4 third order sequences and 12 system tracts. 摘要应用层序地层学方法将川西前陆盆地上三叠统划分为4个三级层序和12个体系域。
- The basement depressions appear at the foreland basin. 盆地边缘的前陆盆地表现为基底深凹；
- Maranon Basin is one of Sub-Andean foreland basins. 秘鲁Maranon盆地是安第斯山山前的前陆盆地之一。
- Based on synthetic investigation date in the western Taiwan Strait in 1984, the characters of vertical distribution of AOU in spring are analysed. 根据1984年台湾海峡西部海域综合调查资料,分析了该海区春季表观耗氧量垂直分布的特征。
- The Chuxiong Basin is a typical foreland basin formed in the Mesozoic. 楚雄盆地为中生代形成的典型前陆盆地。
- Huang, F.W.(1987) Wrench faults in western Taiwan and oil-gas accumulation. Petroleum Geology of Taiwan, 23, 1-12. 黄富文(1987)台湾西部之扭力断层与油气储积。台湾石油地质，第23号，第1-12页。
- Geological characteristics of the coastal zone north and south of the Chouchui Shi River, western Taiwan (Q. L. Lee, Master thesis, 2006). 台湾西部浊水溪河口南北两岸的海岸带之地质特徵(李昆霖、硕士论文、民国95年)。
- Tarim basin is a huge superposed basin composed of Paleozoic cratonic basin and Meso-Cenozoic foreland basin. 塔里木盆地是一个由古生代克拉通盆地与中、生代前陆盆地叠合而成的大型叠合盆地。
- Liew, P.M. and Lai, T.H. (1993) Late Quarternary Evolution of Chou-Shui Fan-delta, Central Western Taiwan, Final meeting of IGCP Project 274, Belgium. 刘平妹,曾美惠,1994,台北盆地五股与板桥井样之花粉学研究,台湾之第四纪第五次研讨会暨台北盆地地下地质与工程环境综合调查研究成果发表会论文集,第234-237页
- The foreland basin of Late Paleozoic is accumulated by the Upper Devonian and Lower Carboniferous. 晚古生代在前陆盆地率先接受了上泥盆统、下石炭统沉积;
- In conclusion, the Lower Cretaceous in Kuqa Depression recorde a whole episode of foreland basin tectonic evolution. 总之，库车坳陷下白垩统记录了一幕完整的前陆盆地构造演化过程。
- Classification, sedimentary and structural features of foreland basin are discussed. 对前陆盆地类型划分、沉积、构造特征进行了研究。
- It is a backland basin of Ailaoshan orogenic belt instead of a foreland basin as some geologists have considered. 它与哀牢山造山带西侧的前陆盆地虽然同时发生，但其形成的沉积环境和岩石组合并不相同。
- Kuqa Depression, located in the North Tarim Basin, is a Meso-Cenozoic foreland basin. 库车坳陷是在南天山海西褶皱带的形成过程中发展起来的中、新生代前陆盆地。
