1) peripheral geosyncline
![点击朗读](/dictall/images/read.gif)
周缘地槽
2) marginal trough
![点击朗读](/dictall/images/read.gif)
边缘地槽
3) open marginal geosyncline
![点击朗读](/dictall/images/read.gif)
陆缘地槽
5) closed marginal geosyncline
![点击朗读](/dictall/images/read.gif)
封闭陆缘地槽
6) peripheral foreland basin
![点击朗读](/dictall/images/read.gif)
周缘前陆盆地
1.
There are three kinds of fore-land basins classified in terms of origin and location:peripheral foreland basin,retroarc foreland basin and regenerated foreland basin.
根据前陆盆地带成因和位置,可以分为3种类型:周缘前陆盆地、弧后前陆盆地和再生前陆盆地。
2.
Along with Tajik Basin and the Southwest Southwest Depression of Tarim Basin, Alay Basin was one of the remnant basins on the north rim of the Tethys during the Late Triassic to Paleogene, it became a peripheral foreland basin in Miocene.
阿莱依盆地是特提斯北缘盆地群中的一个,晚三叠世—古近纪与相邻的塔吉克盆地、塔里木盆地西南坳陷基本连通,中新世以后才成为分隔的周缘前陆盆地。
3.
Dickinson formally introduced the term foreland basin and proposed two geneticclasses:(1)peripheral foreland basin and (2)retro- arc foreland basin.
Dickinson正式引入前陆盆地这一术语并提出周缘前陆盆地和弧后前陆盆地两种成因类型。
补充资料:周缘
1.四周的边缘。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
参考词条