1) Crust mantle structure
壳幔构造
2) crust-mantle structure
壳幔结构
1.
The research on crust-mantle structure is a classical topic of seismology.
对地球壳幔结构的研究是地震学的一个经典课题。
3) crust and mantle structure
壳幔结构
1.
Study on deep crust and mantle structure of the basin,Changling rift controlling skeletal faulting system,shallow and middle CO2 gas reservoir and passing associated mineral dawsonit.
通过盆地深部壳幔结构、长岭控陷骨架断裂体系、中浅层CO2气藏及其伴生矿物片钠铝石分布等研究后发现,乾安大断裂及其延伸部分是孙吴断裂在松辽南部的具体表现形式,规模大,切割深,控制了盆地演化与火山发育,作为联系深、浅物质能量交换的纽带,热流底辟体、地壳内岩浆囊和大型犁式断裂诱发的火山岩在空间上的叠合配置,是松南无机成因天然气分布的主要输导体系。
2.
The differences of the crust and mantle structures in the different spots of this area show the movement and evolution process of deep asthenosphe.
高导层反应出岩石圈中拆离面、滑脱面以及流变塑性带的特性,也揭示出本区大陆壳幔结构。
4) crust-mantle structures
壳-幔结构
1.
Discussion on the Crust-Mantle Structures and Their Formation below the Rift Basins ——Result of the crust-mantle structures below Songliao basin revealed by the near-vertical seismic reflection profiles;
裂谷盆地下的壳-幔结构及其成因机制讨论——以由近垂直反射地震剖面揭示的松辽盆地下的壳-幔结构为例
5) Mantle and earth's crust structures
幔壳结构
6) mantle branch
幔枝构造
1.
The northeast plunging crown of Fuping mantle branch structure occurred the intersection of Wulonggou-Shanghuangqi ductile-brittle shear belts along this mantle branch axis and peripheral main detachment belts.
阜平幔枝构造北东倾伏端 ,是轴部乌龙沟 -上黄旗韧脆性剪切带与外围主拆离滑脱带的交汇部位 ,断裂构造发育 ,岩浆活动强烈 ,成矿控矿有利 ,矿床类型多样。
2.
The main detachment zone system between metamorphic magmatic complex uplift and cover of the periphery of the mantle branch is good for ore-forming and ore-controlling structures.
幔枝构造是地幔热柱多级演化的第三级构造单元 ,其核部变质—岩浆杂岩隆起与外围盖层之间的主拆离带体系是很好的成矿控矿构造。
3.
From a viewpoint of mantle branch tectonics, the deposit is situated at the core of the Da Hinggan Mountains mantle branch, and the multiple evolution of the mantle hot plume linked up the deep hydrothermal ore fluids.
笔者从幔枝构造视角研究认为,矿区位于大兴安岭幔枝构造核部,地幔热柱多级演化沟通了深部含矿流体,并沿途萃取部分成矿物质,在有利的成矿构造裂隙中集聚成矿。
补充资料：壳壳
1.亦作"殻殻"。 2.诚笃貌。 3.中空貌。 4.象声词。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
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