1) back-arc(interarc) basin
弧后(弧间)盆地
2) back arc basin-island arc-interarc basin setting
弧后盆地-岛弧-弧间盆地
3) Back-arc and Interarc Basin
弧后及弧间盆地
4) Inter-arc or back-arc basin
弧间或弧后盆地
5) back arc basin
弧后盆地
1.
In the light of geodynamics and global tectonics,this paper delves into the generation and evolution of Mesozoic Cenozoic back arc basins along the western Pacific active continental margin.
文章以地球动力学和全球构造观点来探讨西太平洋活动大陆边缘中—新生代弧后盆地的基本特征、形成机制、大地构造学涵义和油气藏分布规律。
2.
It is emphasized that,for the different kinds of volcanic rocks in Okinawa Trough,typical active back arc basin in the initial stage of spreading,the study should be based on the modern theory and technique of geochemistry and also on the integrated induction and thinking in view of magmatism in a.
指出应基于现代地球化学理论和方法 ,从板块构造沟弧盆体系岩浆作用的角度 ,将冲绳海槽这一典型幼年期弧后盆地中复杂多变的火山岩作整合型归纳和思考 ,既揭示不同岩石系列的成因联系 ,又注重将岩浆作用与构造环境相结合 ,并在与成熟弧后盆地火山岩的对比中揭示弧后盆地早期扩张过程中岩浆作用的特性、规律与标志 ,以揭示弧后盆地早期扩张的构造动力学过程。
3.
(2) The volcanic rocks in the belt are different from these of typical mid oceanic ridge, and similar to those of back arc basin in lithogeochemical feature.
金沙江造山带一直被当作古板块缝合带，但其物质组成和结构并不反映当时典型的洋盆环境，主要证据有：（１）沉积地层表明，金沙江海盆在规模和水体深度两方面都是有限的；（２）所产的火山岩与标准洋中脊不同，其岩石化学特点与弧后盆地相吻合；（３）澜沧江洋盆与金沙江海盆隔着昌都长条形地块相向俯冲，而且金沙江海盆的俯冲始于澜沧江洋的闭合。
6) back-arc basin
弧后盆地
1.
From the back-arc basin to foreland basin-Ordovician-Devonian sedimentary basin and tectonic evolution in the North Qilian orogenic belt;
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
2.
The volcanic-sedimentary rock that the lower part of the Yanbian Group is deposited in a back-arc basin setting, and the Zagu formation is deposited in a retroarc basin setting based on the analysis of stratigraphy, geochemistry and clastic petrofacies.
通过对盐边群各岩性段地层的产出、构造变形特征及相互间的接触关系的确认,在对碎屑岩组段进行颗粒骨架分析的基础上,结合已有的地球化学和同位素年代学研究结果,盐边群火山岩及其南侧的深成岩均不是蛇绿岩的组份,该火山岩可能形成于弧后伸展环境,盐边群中下碎屑岩段形成于弧后盆地,而上部碎屑岩段则可能形成于前陆盆地。
补充资料：弧剌
1.犹狐剌。形容歪斜不正。
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