1) low-lying land governess
洼地治理
1.
On analysis of the case on the conservation of water and soil on project to important low-lying land governess in Anhui boundaries;
安徽省重点洼地治理工程水土保持方案分析
2) diwa tectonics theory
地洼理论
3) diwa metallogenetic theory
地洼成矿理论
1.
Based upon diwa metallogenetic theory,the division and evolution of geotectonic units in the province were studied in this paper,and there are 2Ⅰ class、3Ⅱ class、7Ⅲ class and 45Ⅳ class tectonic units in the whole province limits.
本文据地洼成矿理论，对省内大地构造单元的划分及演化进行了研究，将其划分为２个Ⅰ级、３个Ⅱ级、６个Ⅲ级、４５个Ⅳ级大地构造单元，认为中生代由于地台活化转入地洼阶段是省内大地构造演化的一大特点。
2.
Based upon the diwa metallogenetic theory, the geotectonic evolution and the characteristics of discovered polymetallic ore deposits included Au, Ag etc.
据地洼成矿理论，对舞钢地穹的大地构造演化和已有的金（银）多金属矿床特征进行了研究，总结了成矿规律和控矿因素。
4) pre-processing method for depressions and flat areas in DEM
洼地平区预处理
5) Diwa
地洼
1.
MINERALIZATION AT TRANSITION ROOM AND ITS SIGNIFICANCE ──Taking Uranium Ore Deposits in the Southeast China Diwa Region as Examples;
地洼区的过渡间成矿及其意义──以东南地洼区铀矿为例
2.
There is a close relationship between occurrence of nonmetallic minerals and tectonic evolution of geosyncline,platform and diwa(geodepression)on the western margin of the Dongting diwa.
洞庭地洼西缘非金属矿产的产出特征与地槽、地台及地洼构造的演化具有密切的关系。
3.
Based upon diwa metallogenetic theory,the division and evolution of geotectonic units in the province were studied in this paper,and there are 2Ⅰ class、3Ⅱ class、7Ⅲ class and 45Ⅳ class tectonic units in the whole province limits.
本文据地洼成矿理论，对省内大地构造单元的划分及演化进行了研究，将其划分为２个Ⅰ级、３个Ⅱ级、６个Ⅲ级、４５个Ⅳ级大地构造单元，认为中生代由于地台活化转入地洼阶段是省内大地构造演化的一大特点。
6) depression
[英][dɪ'preʃn] [美][dɪ'prɛʃən]
洼地
1.
The favorable parts for bonanza ores are beneath clay zones and adjacent to pyrite deposit or in depression and funnel.
成矿盆地斜坡下部的铝土矿带与硫铁矿相邻地段、成矿洼地、凹地及漏斗是铝土矿富矿赋存部位及找矿有利地段。
2.
This algorithm could fast determine disconnected depressions and their influence areas on the basis of acquiring digital tide-coordinates shorelines(DTS).
此算法在提取数字伴潮海岸线(DTS)的基础上,快速确定不连通的洼地及其影响域。
3.
Disconnect depressions are determined depending on types of DTS,and influencing areas of them are computed efficiently.
根据DTS的类型确定不连通的洼地,并快速计算其影响域,同时合理地确定潮滩与水面模型的表达方式,正确构建和显示淹没区。
补充资料：喀斯特洼地
| 喀斯特洼地 karst depression 碳酸盐岩地区因溶蚀作用所形成的负地形。又称溶蚀洼地。包括喀斯特漏斗、喀斯特圆洼地、喀斯特合成洼地、喀斯特槽谷、喀斯特盆地、喀斯特湖等。它是由喀斯特水（指喀斯特地区流水，包括地表水和地下水）垂直循环作用加强或地下洞穴塌陷造成的。洼地的规模主要受集水面积的控制。一般说，地下水的下游，流域面积大，通过洼地的水量大， 洼地的规模也大。洼地规模也与喀斯特水的排泄方式和水平循环的强度有关。此外，还与地壳运动有关，当地壳运动趋于稳定时，洼地趋向扩大。 |
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