弧后前陆盆地

晚三叠世沉积盆地分属周缘前陆盆地、弧前盆地和弧后前陆盆地；

In the Late Triassic , the sedimentary basins are divided into peripheral foreland basin , forearc basin and retro-arc foreland basin .

楚雄弧后前陆盆地的形成及演化

The formation and evolution of Chuxiong back - arc foreland basin

云南思茅三叠纪弧后前陆盆地的沉积特征

The Sedimentary Characteristics of Simao Triassic Rear Arc Foreland Basin , Yunnan Province

弧后前陆盆地是哥伦比亚乃至南美洲勘探的热点地区。

Arc foreland basins are exploration hotspot in Colombia and even in South America .

中&晚奥陶世，塔中东部及塔东地区在构造上具弧后前陆盆地性质。

Tectonically , it is characterestic of a back-arc foreland basin in the eastern Tazhong-Tadong area during the Middle-Late Ordovician .

宁夏中南部地区在中奥陶世至泥盆纪是作为北祁连造山带北侧的弧后前陆盆地靠大陆一侧而存在的；

In the period from Middle Ordovician to Devonian , the central and southern Ningxia area is the back-arc foreland basin in the north continental side of North Qilianshan orogen .

前陆盆地按大地构造位置、发育时间及成因类型等可以划分为周缘前陆盆地、弧后前陆盆地和陆内前陆盆地，新生代库车前陆盆地即属于陆内前陆盆地。

According to geotectonic position , developing time and genesis , foreland basins could be classified into three types : peripheral foreland basin , back arc foreland basin and intracontinental foreland basin .

新疆博格达地区早二叠世软沉积物变形构造：弧后碰撞前陆盆地地震记录

Early Permian seismically induced soft-sediment deformational structures in Bogda region , Xinjiang : stratigraphic records of earthquakes in the retroarc collisional foreland basin

从弧后盆地到前陆盆地北祁连造山带奥陶纪泥盆纪的沉积盆地与构造演化

From the back - arc basin to foreland basin - Ordovician-Devonian sedimentary basin and tectonic evolution in the North Qilian orogenic belt

竟柱山组沉积-火山岩的形成环境揭示了比如盆地的性质在晚白垩世已由弧后盆地转换为前陆盆地。

The Biru Basin developed into a foreland basin during the Late Cretaceous .

晚泥盆世到三叠纪（古特提斯洋阶段），塔西南边缘经历了陆内裂谷/被动大陆边缘盆地-弧后伸展盆地-弧后前陆盆地发展旋回；

From Late Devonian to Triassic , the period of paleo-Tethyan ocean ocean , the southwestern margin of Tarim experienced the developmental cycle of intracontinental rift / passive epicontinental basin-back-arc extensional basin-back-arc foreland basin .

第三纪，西湖凹陷经历了弧后盆地、残余弧后盆地至前陆盆地的发展过程。

Tertiary period , Xihu Sag had experienced basinal evolution from back-arc basin , relict of back - arc basin to foreland basin .