1) local deposition
局域沉积
1.
CO 2 laser-induced local deposition of silver from aqueous solution was explored .
探讨了CO2 激光诱导液相局域沉积银的过程。
2) liquid-phase local deposition
液相局域沉积
1.
And CO 2 laser, whose output laser wavelength is in middle infrared, is also very difficult to achieve liquid-phase local deposition of metal on the right side of the substrate by the conventional methods.
而对于输出波长在中红外波段的CO2 激光器 ,运用常规的方法 ,也不易实现金属在试片正面的液相局域沉积。
3) sedimentary framework
沉积格局
1.
Based on the analyses of the late Mesozoic sedimentary framework, structural deformation, and of late Jurassic-early Cretaceous magmatic and thermal events in the basin and its adjacent regions, it is suggested that the basin prior to the late Jurassic was mainly controlled by Tethys tectonic domain, whereas influenc.
通过晚中生代及其周缘地区沉积格局、构造变形、晚侏罗世—早白垩世的岩浆及热事件的分析 ,认为晚侏罗世以前盆地主要受特提斯构造域的控制 ,古太平洋板块对盆地格局的影响在晚侏罗世晚期以后才有所表现。
2.
The understanding and definition of the sedimentary framework in this area are directly related with exploration deployment in the northeastern part of Sichuan basin.
由于对该区沉积格局的认识和确定直接涉及川东北地区的油气勘探部署。
3.
The sedimentary framework of the Zhoukou depression during Early Cretaceous time has been ascertained on the basis of the study of provenances, palaeotopography, palaeocurrent,water media and palaeoclimates.
本文在讨论了湖盆的物源、古地形、古水流、水介质条件及古气候条件的基础上，提出了早白垩世时周口坳陷的沉积格局。
4) depositional system tract
沉积体系域
1.
Having analysed seismic, drilling and crop data of Carboniferous system in the Tarim basin, we divide Carboniferous system into three sedimentary sequences (CⅠ、 CⅡ、 CⅢ ) or eight depositional system tracts (CⅠ1、CⅠ2、C3、 CⅡ1、 CⅡ2、 CⅡ3、 CⅢ1、 CⅢ2 ).
根据塔里木盆地有关石炭系地层的地震资料、钻井资料和露头资料，将其分为3个三级沉积层序（CⅠ、CⅡ、CⅢ）和8个沉积体系域（CⅠ1、CⅠ2、CⅠ3、CⅡ1、CⅡ2、CⅡ3、CⅢ1、CⅢ2）。
2.
Six types of depositional system tracts occurs in different developing period of the graben.
地堑内主要发育冲积扇体系、扇三角洲体系和湖泊体系，在地堑不同演化阶段分别构成６种沉积体系域类型。
5) sedimentary basin tract
沉积盆地域
1.
On the basis of analysis for the character of stratigraphic interface and the depositional architecture of genetic stratigraphic units, the stratigraphic sequence of Permian to Trassic is divided into seven depositional episodes, three tectono-depositional episodes and two sedimentary basin tracts, and the evolutional cours.
在分析地层界面性质和各类成因地层单位沉积构成的基础上,将华南二叠-三叠系划分为7个沉积幕、3个构造沉积幕和2个沉积盆地域,恢复了华南板块二叠-三叠纪的演化过程,论述了板块构造运动、海平面升降和源区侵蚀作用对各级成因地层单位的控制意义,证明了华南的古特提斯海经历了陆表海和伸展裂谷海两个演化阶段。
6) Local close packing
局域密堆积
补充资料：超导电性的局域和非局域理论（localizedandnon-localizedtheoriesofsuperconductivity）
超导电性的局域和非局域理论（localizedandnon-localizedtheoriesofsuperconductivity）
伦敦第二个方程（见“伦敦规范”）表明，在伦敦理论中实际上假定了js(r)是正比于同一位置r的矢势A(r)，而与其他位置的A无牵连；换言之，局域的A(r)可确定该局域的js(r)，反之亦然，即理论具有局域性，所以伦敦理论是一种超导电性的局域理论。若r周围r'位置的A(r')与j(r)有牵连而影响j(r)的改变，则A(r)就为非局域性质的。由于`\nabla\timesbb{A}=\mu_0bb{H}`，所以也可以说磁场强度H是非局域性的。为此，超导电性需由非局域性理论来描绘，称超导电性的非局域理论。皮帕德非局域理论就是典型的超导电性非局域唯象理论。
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