1) Rb-Sr isochron
Rb-Sr等时线
1.
The effect of different crust-mantle mixing environments on Rb-Sr isochron ages is discussed in terms of a two-component mixing model.
本文利用二元混合模型讨论了壳幔物质的不同混合环境对Rb-Sr等时线年龄的影响。
2.
The paper deals mainly with temperature-pressure geochemistry characteristics, hydrogen and oxygen isotope composition as well as the Rb-Sr isochron ages of fluid inclusions in mass of rock and orebody in the Dabao Shan polymetallic deposit.
本文拟据大宝山矿床包裹体温压地球化学特征和氢、氧同位素以及矿物流体包裹体Rb-Sr等时线年龄的系统研究,认为成矿物质主要来源于岩浆期后含矿热液,其成因应属于燕山早期岩浆期后热液矿床。
2) Rb-Sr isochron age
Rb-Sr等时线年龄
1.
The sphalerite gives an Rb-Sr isochron age of 486 Ma±,showing that the deposit formed in the Caledonian stage.
对闪锌矿进行了Rb-Sr等时线年龄测定,获得马元锌矿的成矿年龄为486Ma左右;根据对矿物C、H、O、S同位素和微量、稀土元素的研究,认为该锌矿的成矿物质来自围岩地层。
3) Rb Sr mineral isochron
Rb-Sr矿物等时线
4) Rb-Sr whole-rock isochron
Rb-Sr全岩等时线
5) Rb Sr isochrone dating
Rb-Sr等时线定年
6) quartz vein Rb-Sr dating
石英脉Rb-Sr等时线年龄
补充资料：时为
1.犹专为，单为。
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