例句與造句

1. Plate tectonic analysis of basin systems interspersed in orogenic belts requires that the effects of approximation be carefully distinguished from those of separation .
   分析造山帶中盆地系的板塊構(gòu)造時(shí)，需要將靠近作用與分離作用仔細(xì)區(qū)分開來(lái)。
2. At the same time , attained following fruits : 1 . the tectonic analysis indicated that the distortion of the foreland basin was mainly attributed to the movements of longmen mountains , the structural features , forming periods , and transformation fashions are different between the northern and southern segments
   主要取得如下成果： 1 、構(gòu)造研究表明川西坳陷形成與形變主要受控于龍門山造山帶，表現(xiàn)為坳陷內(nèi)部南、北段構(gòu)造特征、形成期及其變形方式上的差異。
3. Basing on the acquaintence of the stratum , the rock , the structural setting , the tectonic framework and the research in the stratum , the rock and the structure of dam area in detail , using the modern principle of tectonic analysis , this paper analyzes the geometry characteristics , the deformation characteristics , the dynamics characteristics , kinematics characteristics of the dislocation interfaces . further more this paper discuss " the structural generation , the structural sequence and the structural evolution of the dislocation interfaces
   在了解區(qū)域地層、巖石、構(gòu)造背景和格局等基礎(chǔ)上，結(jié)合對(duì)壩區(qū)地層、巖石和構(gòu)造的詳細(xì)調(diào)查研究，采用現(xiàn)代構(gòu)造解析的原理和方法，對(duì)壩區(qū)錯(cuò)動(dòng)帶幾何學(xué)特征、變形特征、動(dòng)力學(xué)特征和運(yùn)動(dòng)學(xué)特征進(jìn)行了全面的分析，并在此基礎(chǔ)上探討分析了壩區(qū)錯(cuò)動(dòng)帶的構(gòu)造世代、變形序列及構(gòu)造演化。
4. Based on the theory of plate tectonics and the new knowledge of continental dynamics , this paper starts mostly with tectonic analysis and then makes a comprehensive view on the characteristic of stratum composition , gold mine mineralized , magmatic activity as well as ruptures activity to discuss the yanshanian tectonic evolution of the xiaoqinling area under the regional tectonic framework of qinling orogenic belt
   本文以板塊構(gòu)造理論和大陸動(dòng)力學(xué)研究的新認(rèn)識(shí)為指導(dǎo)，采用以構(gòu)造分析為主線，結(jié)合區(qū)內(nèi)地層沉積、金礦成礦、巖漿活動(dòng)以及南北兩側(cè)斷陷盆地形成演化等綜合分析，在秦嶺區(qū)域構(gòu)造大框架下對(duì)小秦嶺燕山期的構(gòu)造演化特征進(jìn)行探討。
5. Tectonic analysis controlling gold mine mineralization in taihua group suggest that ductile fractures chang into brittle - ductile ones going with upliftling of xiaoqinling area after in - china orogeny . brittle fractures form on the basis of brittle - ductile ones that develop and inherit the characteristic of the latter stress field . folds and faults analysis in taihua group and its bilateral reveal that yanshanian tectonic evolution of xiaoqinling area undergo at least three phases of deformation
   太華群內(nèi)金礦成礦構(gòu)造分析表明，印支期碰撞造山后小秦嶺擠壓抬升，控礦韌性剪切帶向脆韌性轉(zhuǎn)化( 207 148ma ) ，在脆韌性剪切帶基礎(chǔ)上疊加改造形成容礦斷裂，脆性斷裂的發(fā)育繼承了韌脆性剪切帶發(fā)育時(shí)的應(yīng)力場(chǎng)特征。
6. It's difficult to find tectonic analysis in a sentence. 用tectonic analysis造句挺難的
7. Through the all - sided tectonic analyses , it can be deduced that there are two aspects will be the hidden defects to the dam and the engineering stability of the reservoir area . one is the dislocation interfaces resulting from the the majiaheba faultage ' s thrusting overriding and other causes of formation . the second is the region of strong deformation , such as the above of the dam , middle and high positions of the lava layers and the regions of overprint of the structure of ne to the one of nw , which should be taken into account especially
   通過(guò)區(qū)域和壩區(qū)錯(cuò)動(dòng)帶的全面構(gòu)造解析，認(rèn)為由馬家河壩斷層逆沖推覆作用而在壩區(qū)形成的向金沙江下游緩傾的錯(cuò)動(dòng)帶以及其它成因的錯(cuò)動(dòng)帶是壩區(qū)和庫(kù)區(qū)工程穩(wěn)定的隱患，尤其是變形較強(qiáng)的壩址區(qū)上游區(qū)、中高層位以及北西向構(gòu)造期的錯(cuò)動(dòng)帶疊加于北東向構(gòu)造期錯(cuò)動(dòng)帶的部位，更應(yīng)該引起足夠的重視。