1) standard layer
标准层
1.
The process for predicting fault location by using accoustic abnomality in standard layer includes two stages.
在用标准层声波时差异常法确定断层的位置时，首先对标准层声波时差进行趋势面分析，然后再分析残差等值线图。
2.
This paper proposes a method of using the standard layer to identify deep gas zone in volcanic,with which the effect of lithology,shale vol- ume and well bore can be eliminated,and the difference between gas zone and standard layer can protrude and magnify the gassy informa- tion of the formation.
本文提出视标准层差值法识别深层火山岩气层,该方法消除岩性、泥质和井眼的影响,突出气层与标准层的差别,放大地层含气信息。
4) key bed
标准层
1.
Based on the combination of the key bed and morphological feature of logging curve and formation thickness, a new understanding suggests that the Putaohua oil reservoir changed thinner from west to east and from north to south generally.
根据该地区葡萄花油层顶部、底部砂岩和湖泛泥岩标准层的测井曲线形态特征,结合地层厚度变化,认为葡萄花油层为条带状河道砂体和透镜状河口坝砂体,总体由西往东、由北往南逐渐减薄,油藏形成主要受继承性断裂背斜带控制,平面油水分布明显受断层控制,油藏类型属于构造 岩性型,岩性因素使油藏进一步复杂化。
5) standard event sequence
标准层序
6) stratified standard
分层标准
补充资料：德国国家标准(见德国标准化学会、德国标准体系)
德国国家标准(见德国标准化学会、德国标准体系)
National Standards of Germany: see Deutsches Institut für Normung, DIN;standards system of Germany
Oeguo Guol心日icozhun德国国家标准(Natio.吐S加Ln山切曲of Gen”旧ny)见德国标准化学会;德国标准体系。
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