1) Wa60-H26 Well
洼60-H26井
1.
Wa60-H26 Well is a medium-curvature horizontal well with panned depth of 1922 m.
洼60-H26井是一口中曲率水平井,设计井深1 922 m,由于地面条件的限制,设计采用三维井眼轨道。
2) Wa 38 well area
洼38井区
3) Jing erwa Formation
井儿洼组
5) Jing erwa profile
井儿洼剖面
1.
The lamina samples of Jing erwa profile in Nihewan Basin, which are deposited in the form of silt-clay couplet, are studied by scanning electron microscopy (SEM) and X-ray energy dispersive spectrum (EDS).
利用扫描电镜以及X射线能谱仪 ,对泥河湾盆地井儿洼剖面的粉砂黏土沉积纹层进行成分分析 ,结果表明在一个纹层偶中Si和Ca元素的质量含量w存在明显的差异 ,粉砂纹层中的w(Si)值高 ,w(Ca)值低 ;而黏土纹层中的w则正好相反 。
6) 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。
补充资料：分散紫 26
分子式：C26H18N2O4
分子量：422.43
CAS号：6408-72-6
性质：密度1.385。熔点195°C。
分子量：422.43
CAS号：6408-72-6
性质：密度1.385。熔点195°C。
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