遥感分析的过程就是一个定量反演的过程。
The essence of remote sensing is a process of quantitative inversion.
提出了定量反演三维断层参数(上顶深、断距等)的方法。
We put forward an inversion method of 3D fault parameters (the top deep and the fault displacement etc) of the quantitative interpretation.
本文的目的是对青藏高原地表反照率和冷热源参数进行定量反演。
The objective of this paper is to retrieve the albedo of the plateau and then to calculate the parameters about hot or cold source quantitatively.
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