1.
An Oblique Cross Section of Archaean Continental Crust in Shanxi Hebei Nei Mongol Jnnctnve Area, North China Craton
太古宙克拉通型下地壳剖面：华北怀安－丰镇－尚义的麻粒岩－角闪岩系
2.
Seismic sections show the response of the earth to seismic waves.
地震剖面是地壳对地震波的响应。
3.
hydrogeochemical profile
地下水水化学剖面图
4.
Stable Isotope and the Sedimentation of Shell Bar Section from Qaidam Basin;
柴达木盆地贝壳堤剖面稳定同位素与沉积环境
5.
CHARACTERISTICS OF THE DENSITY STRUCTURE OF THE CRUST AND UPPER MANTLE IN LUYANG-HAICHENG DONGGOU DSS PROFILE
闾阳—海城—东沟剖面地壳与上地幔密度结构特征与地震
6.
Sub-bottom profiling technology for detecting underwater root-stone in Yellow River
黄河水下根石探测的浅地层剖面技术
7.
Study on the Method of Auto-draw Slice Geological Profile in MapGIS
MapGIS下图切地质剖面自动绘制方法探究
8.
RESERVOIR CHARACTERISTICS OF THE ORDOVICIAN WEATHERING CRUST AND SECTIONAL STRUCTURE IN ORDOS NO.7 WELL,THE ORDOS BASIN
鄂尔多斯盆地鄂7井奥陶系风化壳储层特征与剖面结构
9.
Organic Biomakers and the Sedimentation of Shell Bar Section from Qaidam Basin
柴达木盆地贝壳堤剖面有机分子化石与沉积环境
10.
The crust under ocean deeps would be thinner than under land surfaces at or near sea level.
深海下面的地壳比海平面或者接近海平面的陆地下面要
11.
The application of the sub-bottom profile technology on footstone detection in the lower Yellow River
浅地层剖面技术在黄河下游根石探测中的应用
12.
The crustal thickness from East China Sea to North Fiji Basin was calculated on the basis of the actually measured water depth and the gravimetric data from continuous profiling.
根据我们实测的水深、重力连续剖面资料,计算了自东海至北斐济盆地的地壳厚度。
13.
The Dynamic Response of Folding Double-Layer Cylindrical Reticulated Shell;
折叠式双层柱面网壳在地震作用下的动力响应
14.
DYNAMIC CAPACITY RESEARCH OF THE SINGLE-LAYER SPHERICAL LATTICE SHELLS UNDER MULTI-DIMENSION EARTHQUAKE INPUTS;
多维地震作用下单层球面网壳的动力性能研究
15.
Dynamic response analysis of the single-layer latticed cylindrical shell in effect of earthquake
在地震作用下单层柱面网壳的动力响应分析
16.
Seismic response analysis of spherical shells under multiple support excitation
多点输入下球面网壳结构地震响应研究
17.
Like the earth, the moon is in layers, with a crust on the outside and a deep mantle below.
如同地球一样，月球上有地层，表面是一层地壳，其下是很深的地幔。
18.
Subsurface structures have been obtained through regional deep seismic profiles and kinematic data recovered from nearly continuously cores.
通过区域深反射剖面和近于连续的岩心样品数据，已经获得了地下的精细结构剖面。