1) focal depth
震深
2) deep earthquake
深震
1.
Comparative analysis of phase characteristics and seismic factors of the deep earthquake on Northeast China;
对东北深震震相特征和地震参数的对比分析
2.
Study on the dynamic features of subsurface fluid precursor before Huichun M7.0 deep earthquake;
珲春7.0级深震地下流体前兆的动态特征研究
3.
Study on the subsurface fluid anomalies before Wangqing Ms7.2 deep earthquake;
汪清7.2级深震地下流体动态异常探析
3) deep seismic sounding
深地震测深
1.
According to the results of the deep seismic sounding and surface wave dispersion tomography, a two-dimensional model is used to do the match in the interpretation.
解释时根据深地震测深和面波频散层析成像的结果，用二维模型进行正演拟合。
2.
We give a method for use as the data of deep seismic sounding which identifies and calculates the uncertainty automatically in phase picking.
本文给出了一个主要用于深地震测深数据的震相识别误差(不确定性)的判别和计算方法。
3.
The Benzilan-Tangke deep seismic sounding profile in the western Sichuan region passes through the Songpan-Garze orogenic belt with trend of NNE.
位于川西地区的奔子栏—唐克深地震测深剖面以NNE走向穿越松潘—甘孜造山带 。
4) seismic sounding
地震测深
1.
A seismic sounding profile crossing the eastern Qinling Mountain was performed in the Western Henan Province, China.
对横穿秦岭东段的人工地震测深剖面进行二维射线追踪处理，得到了该剖面上的二维速度结构图。
2.
The structural analyses of many seismic sounding profiles indicate that there are two fault systems in China continental lithosphere, which are different obviously and correlative closely: one is the shallow fault system composed of ductile-brittle shear zones mainly in surface crust, and the other is deep fault system mainly composed of crust-mantle ductile shear zones, which cuts the Moho.
众多地震测深剖面的地质构造解析显示,大陆岩石圈存在既有显著差异又有密切联系的两套断裂系统,即以地壳表层脆性剪切带为主的浅层断裂系统和以切割莫霍界面的壳幔韧性剪切带为主的深部断裂系统。
3.
A crustal thickness and velocity structure model of continental China has been constructed based on a systematic structural analysis of the seismic sounding profile in continental China and its adjacent regions.
通过中国大陆及邻区地震测深剖面的系统构造解析,建立起中国大陆岩石圈地壳厚度与速度结构模型。
5) Deep seismic sounding
地震测深
1.
A genetic algorithm of body waveform inversion is presented for better understanding of crustal and upper mantle structures with deep seismic sounding waveform data.
为了更好地利用地震测深波形数据,提出了地震体波波形反演的遗传算法。
2.
D crustal velocity structure and vP/vS are obtained by processing and interpretation of S-wave data from Maqin-Jingbian deep seismic sounding (DSS) profile.
对玛沁—靖边剖面深地震测深S波资料处理解释,获得本区S波二维地壳速度结构和波速比结构。
3.
Observational data from some of the 10-odd deep seismic sounding (DSS) profiles in Bohai Bay and its adjacent areas were processed with the methods of two-dimensional (2-D) ray tracing, travel-time fitting and synthetic seismogram.
利用渤海湾及其邻区的10多条地震测深剖面段观测资料,对部分剖面进行二维射线追踪、走时拟合及合成地震图计算,获得了本区地壳上地幔速度结构。
6) focal depth
震源深度
1.
The spatial and temporal distribution of focal depth before strong shocks in Yunnan;
云南地区强震前震源深度的时空展布
2.
A PTD method a new method for determinating focal depth and its application;
确定震源深度的PTD方法及其应用
3.
We used the catalog of Earthquake Administration of Xinjiang and HYPODD to analyze the characteristics of focal depth and its tectonic significance in Urumqi region,Xinjiang.
采用新疆维吾尔自治区地震局精度较高的常规地震目录和双差定位目录,对乌鲁木齐地区震源深度的分布特征及与断层的关系进行了研究。
补充资料：热深厥深
热深厥深 热深厥深 病证名。指热厥证的征象。指邪热越深入，四肢厥冷的症状越严重，皆因阳气被遏，邪气内闭所致。属真热假寒证。
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