1) Activated deep tectonics
深部构造活化
2) deep structure
深部构造
1.
The special bouguer gravity fields and the deep structure in yinshan-daqingshan mountains;
阴山大青山山系特异重力场与深部构造
2.
The feature of deep structure in the area is revealed, and the deep metallogenesis is discused.
本文中利用重力、航磁和深部地球物理剖面资料,解析研究区三维岩石圈结构,揭示深部构造特征,进而探讨深部成矿作用。
3.
By analysing and studying aeromagnetic and gravity anomalies and theirtransformed results,this paper explains the distributing characteristics of deep structures,such as folds and fauIts,granite bodies,the Archean coplex in Qingyuan area and therelations between these deep structures and gold deposits.
通过航磁、重力异常及数据处理成果的分析和研究，阐述了清原地区深部构造、区域构造、花岗岩体及太古宙变质杂岩的展布特征与金矿成矿之间的关系，指出了该区金矿成矿的远景地段。
3) Deep-seated structure
深部构造
1.
A preliminary interpretation on the deep-seated structure of the Longgang compound landmass;
龙岗复合陆块深部构造浅析
2.
On this basis, the authors focused on the upper mantle lithosphere-asthenosphere structure of eastern China, and concluded the following: (1)seismic tomography images can diotinguish between Mesozoic and Cenozoic deep-seated structures,using di.
文中以地震层析原始数据为基础,结合大地电磁测深和热流值数据,对老资料重新开发,编制了中国东部岩石圈厚度图、大地热流值图、岩石圈构造与矿集区关系图等,在此基础上对中国东部上地幔岩石圈-软流圈构造及其变异进行了初步研究,认为:(1)中生代燕山期较大型深部构造(如软流圈上涌体)的地震层析影象可存留至今,运用大地热流值及其相应浅表岩浆岩、矿集区等特征差异可以将中、新生代深部构造加以区分;(2)中国东部深部构造总特征:上地幔岩石圈-软流圈构造起伏变化,岩石圈西厚东薄,软流圈上涌发育且形式各异。
3.
Based on the great change of the lithosphere thickness,the geothermal flow and Moho surface,and epigenetic magma structure activities,the sketch map of deep-seated structure of North China is constituted,and the relationship model of Yanshanian upwelling of asthenosphere and lithosphere structural activity is built.
通过岩石圈厚度变化、大地热流值和莫霍面起伏,结合浅表岩浆构造活动,编制了华北地区深部构造略图,建立了燕山期软流圈上涌与岩浆构造活动的关系模式,总结了该区的深部构造特征:岩石圈厚区与软流圈上涌区共存。
4) deep structures
深部构造
1.
Geophysical characteristics of TanLu fault zone reveals its deep structures.
地球物理特征揭示郯庐断裂带深部构造,为研究重点矿产分布规律及地震灾害预报具有重要的实际意义。
5) the deep-shallow structures
深浅部构造
6) activated tectonics
活化构造
1.
Some geodynamic issues concerned in activated tectonics (Diwa) theory, initialized by Academician Chen Guoda in 1950 s, are systematically reviewed and discussed in this paper to celebrate and rememorize his outstanding contribution and achievement in Earth Sciences.
本文从地球物理角度出发,以物理概念和数学描述相结合的定量方式,对陈国达院士生前所创建的活化构造(地洼)理论研究中的某些地球深部动力学问题进行了较系统的综合评述和探讨。
补充资料：白银有色金属公司深部铜矿主井和副井
白银有色金属公司深部铜矿主井和副井
白银有色金属公司深部铜矿主井和副井
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