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楚雄盆地的性质属弧后前陆盆地。The Chuxiong basin is a back-arc foreland basin.

前陆盆地是研究造山运动的关键地区之一。Foreland basins are the key areas for the study of orogeny.

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大巴山前陆构造发育多套烃源岩。Source rocks are widely developed in foreland of Daba Mountains.

简述了国外前陆盆地研究的新进展。Making new progress on the research for foreland basin is outlined.

造山带和克拉通之间的盆地称之为前陆盆地。The basin between orogenic belt and craton is called foreland basin.

楚雄盆地为中生代形成的典型前陆盆地。The Chuxiong Basin is a typical foreland basin formed in the Mesozoic.

植物根系的模拟是目前国内外研究的前沿问题。Simulation of plant root systems is a internal and overseas research foreland.

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库车坳陷位于塔里木盆地北部,为一前陆坳陷。Kuche Depression, a foreland depression, is situated in the northen Tarim Basin.

为什么沿海地区人的身高比内地、山区人高?。Why is the height of foreland person taller than inland, a mountainous area person?

前陆冲断带普遍具有构造分段的特点。The foreland thrust belt has a characteristic of structural segmentation in general.

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。Kuqa Depression, located in the North Tarim Basin, is a Meso-Cenozoic foreland basin.

目前的研究前沿主要集中在叠前深度域和弹性波。The leading research foreland mainly focuses on pre-stack depth domain and elastic wave.

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乌什凹陷为中新生代两期前陆盆地叠加形成的叠合盆地。Wushi Sag is a superimposed basin of two stage foreland basins of Mesozoic and Cenozoic.

在海相沉积之后接受了陆相沉积,中生代盆地环特提斯洋分布,属南前陆盆地带。Mesozoic basins are distributed around Tethys and belong to southern foreland basin zone.

而其中的生态风险评价更是环境评价研究的一项前沿课题。And one of it' s branches-ecological risk assessment is the foreland of this research field.

晚二叠世末,该地区变成弧后盆地,进一步转化成前陆盆地。The late Permian it was changed into the back arc basin, and transformed into foreland basin.

增加的建设及交通用地主要集中在月湖以西的成山镇附近和以东的沿海地区。Most of the buildings and highways are distributed nearby the Chengshan Town and the foreland.

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随着周缘界山的隆升,准噶尔盆地形成三大前陆盆地系统。With the uplift of marginal mountains, three foreland basin systems were formed in Juggar basin.

库车前陆盆地具有典型的双超压体系。There are two overpressure systems, lower and upper overpressure systems, in Kuqa foreland basin.

塔西南坳陷是一个经长期发展形成的复合型前陆坳陷。Southwest depression in Tarim basin is a complex foreland type as a result of long-term evolution.