1)  Basin-Range Coupling
盆山藕合
2)  basin-mountain
盆山
1.
From a quantitative and semi-quantitative research on Fenwei rift valley system,we suggest that basin-mountain dichotomy of the rift valley system was formed under a regional extensional stress field.
试图运用盆山耦合等地学理论,对汾渭裂谷系进行初步的定量半定量研究。
3)  basin-mountain coupling
盆山耦合
1.
Structural feature and basin-mountain coupling analysis of North Sichuan Basin;
四川盆地北部构造特征及盆山耦合分析
2.
Recently, the research of basin-mountain coupling has become one of the hotspots in Geology.
近年来盆山耦合已经成为地质学研究的热点之一。
3.
The relationship between basin-mountain coupling process and metallogeny is a hot spot in modern geological research.
柴北缘盆地—造山带体系在西北地区有一定的代表性,盆山耦合过程与成矿的研究是当代地质科学研究的热点之一。
4)  basin-mountain system
盆山体系
1.
Integrating study the relationship between basin-mountain system and oil and gas pool forming process is one of the frontier research fields in the study of continental geodynamics,and also is a key problem of petroleum exploration in China.
盆山体系与油气成藏作用的综合研究是当前大陆能源和盆地动力学探索的热门,也是中国油气勘探取得突破的一个关键性问题。
2.
Therefore, analysis of the architecture and tectonic evolution of the basin-mountain system in Sichuan Basin and its adjacent areas would be very important to gain a deeper understanding of the tectonic framework of and petroleum reservoir distribution in Sichuan basin.
盆山体系研究是当前大陆动力学探索的热门。
5)  Basin-range coupling
盆山耦合
1.
Basin-range coupling and lithosphere structure between the Zoigê and the west Qinling;
若尔盖与西秦岭地震反射岩石圈结构和盆山耦合
2.
Evolution of basin-range coupling in the Yunkai Dashan-Shiwan Dashan area, Guangdong and Guangxi: with a discussion of several tectonic problems of South China Geological Bulletin of China,;
两广云开大山—十万大山地区盆山耦合构造演化——兼论华南若干区域构造问题
6)  coupling process between basin and mountain
盆-山耦合
1.
The sequence structure and evolution of both sequences have clearly reflected the coupling process between basin and mountain of the Xujiahe Formation of Upper Triassic in the northeastern Sichuan foreland basin.
此二个级别的层序结构和演化序列,较为清晰地反映了川东北前陆盆地晚三叠世须家河期盆-山耦合过程,特点为:须二段—须三段"下成盆"期米仓山-大巴山造山带以低幅隆升为主,对应的川东北坳陷沉降幅度小,物源供给与可容纳空间增长率稳定和基本持平,以发育辫状河三角洲-湖泊沉积体系为主,其层序结构以上升与下降相域厚度近于相等的对称型为主,反映地层基准面相对稳定和均衡的盆-山耦合过程;须四段—须六段"上成盆"期米仓山-大巴山开始进入强烈逆冲推覆和构造隆升阶段,川东北前陆盆地坳陷幅度急剧加大,碎屑物供给量骤然和增多至远大于可容纳空间增长率,以发育冲积扇-扇三角洲-辫状河三角洲等粗碎屑岩为主的沉积体系为主,其层序结构以上升相域厚度大于下降相域的不完全对称型,在造山带前缘则以发育仅保留上升半旋回沉积记录的非对称型结构为主,反映地层基准面升、降变化大的非均衡盆-山耦合过程。
参考词条
补充资料：藕合
1.亦作"藕荷"。 2.浅紫而微红的颜色。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。