绿砂岩（green sandstone）是砂岩的一种，可作为亚光石材，不会产生因光反射而引起的光污染，又是一种天然的防滑材料。
本文对松辽盆地南部泉头组砂岩中的绿鳞石进行了较为系统的鉴定。
In this paper, celadonite has been proceed expertise of systematically identified in the sandstones of Quan Tou Formation, South Songliao Basin.
立面设计主要通过三种不同的材料表达“像素”的概念：玻璃像素、砂岩像素和绿植像素。
Thee facades "pixels" consist of three primary material types: glass pixels, sandstone pixels, and vegetated pixels.
古氧化绿色砂岩主要由与油-气二次还原作用有关的绿泥石化和绿帘石化造成。
The greenish color of the palaeo-oxidized sandstones mainly results from chloritization and epidotization related to oil and gas secondary reduction processes.
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