周缘前陆盆地

文章认为，曾母盆地是发育在块体会聚带上的周缘前陆盆地；

The article considered that the Zengmu basin is a peripheral foreland basin developed in block of convergent belt ;

云南楚雄盆地位于扬子陆块的西南边缘，为一典型的中生代周缘前陆盆地。

The Chuxiong Basin in Yunnan on the southwestern margin of the Yangtze landmass is a Mesozoic peripheral foreland basin .

碰撞造山带与周缘前陆盆地；

Continental collision orogenic belts and peripheral foreland basins ;

欠补偿周缘前陆盆地发育于陆间造山带的早期阶段。

Underfilled peripheral foreland basins develop in the initial stage of intercontinental orogenic belts .

南秦岭泥盆纪：周缘前陆盆地和新生海洋盆地并列

South Qinling in the devonian : juxtaposition of peripheral foreland basins and new-born oceanic basins

标定碰撞构造的地层学线索&欠补偿周缘前陆盆地结构与充填序列

Stratigraphic constraints on collision tectonics ∶ architecture and filling sequences of underfilled peripheral foreland basins

周缘前陆盆地联合阶段，此时发育了西缘和东北缘两个前陆盆地；

Foreland baSin combination period in which two foreland basins in western margin and northeastern margin formed ;

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 .

与弧背前陆盆地和周缘前陆盆地相并列，并对应于板块构造演化历程中的大洋消减、大陆碰撞和陆内缩短三个不同性质的聚敛阶段。

Therefore they are corresponding to the three different featured convergent stages of ocean subduction , continental collision and intra-continent contraction in the structural evolution of plates .

重建的地层层序和沉积地质特征显示巴颜喀拉盆地主体三叠系复理石沉积是周缘前陆盆地。

The stratigraphic sequences and sedimentological characteristics indicate that the main body of Bayan Har Basin is composed of Triassic flysch sediments deposited in a foreland basin during Triassic .

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。

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 .

以盆地所处的地球动力学环境为基础，将前陆盆地分为周缘前陆盆地、弧背前陆盆地和分裂前陆盆地三类。

The foreland basin , on the basis of its geodynamic environment , can be subdivided into three types of peripheral foreland basin , retro-arc foreland basin and broken foreland basin .

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 .

南海东北部陆缘区新近纪早期反转构造特征及其动力学意义黔西南地区三叠纪周缘前陆盆地沉积相特征

Inversion structure features and their dynamic significances in Early Neogene strata at continental margin of the northeast South China Sea The Sedimentary Facies in Marginal Foreland Basin of Triassic Age in Southwestern Guizhou

结果显示，晚三叠世巴颜喀拉山群物源主要来自大洋岛弧，少量来自大陆岛弧，表明当时研究区处于邻近大洋岛弧的周缘前陆盆地环境。

The result of this research indicates that the tectonic setting where the provenance is most from the oceanic island arc and a few from the continental island arc , the studying area is a basin round oceanic island arc .

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。

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 .

中秦岭前陆盆地位于扬子北缘的边缘，是秦岭洋闭合后的产物，形成于440Ma，结束于323Ma，历时107Ma，属周缘前陆盆地；

Central Qinling foreland basin formed from 440 Ma to 323 Ma , lasted 107 Ma , located in the edge of north margin of Yangtze landmass and is the outcome of the Qinling Ocean basin when closed , referred to as a peripheral foreland basin ;