古代瓷窑。在浙江温州西山。东晋时烧制青瓷，胎为灰色和淡土黄色，质较松。釉肥厚，以淡青为主，少细开片。装饰上多在器物内外刻划莲瓣纹，也有青褐加褐彩的。深口宽底高碗为其典型作品。西山窑在唐、五代和宋时，继续烧造青瓷。
通过沉积基础图件、沉积环境的分析明确了研究区西山窑组沉积演化特征。
Through the base deposition maps, the analysis of sedimentary environment, defined the Xishanyao formation's characteristics of sedimentary evolution.
“杂色泥岩”上覆的白垩系清水河组为超覆，下伏的侏罗系西山窑组被削截。
The Cretaceous Qingshuihe Formation overlaps the variegated mudstone, while the Jurassic Xishanyao Formation is truncated by the variegated mudstone.
台北凹陷是吐哈盆地的主要含油气区，而西山窑组煤系地层是该地区的主力烃源岩。
The Taibei Depression is the main oil and gas bearing area of Tuha Basin, and the coal bearing stratum of the Xishanyao Formation is the most important source rock in the area.
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