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金华盆地位于浙江省中部,是浙江境内最大的内陆盆地——金衢盆地的一部分。但其本身仍是一封闭的向斜盆地。盆地南、北部边界主要为上侏罗统的火山碎屑岩构成的中低山;东西外延邻接鞋塘,白龙桥向斜。金华江横贯盆地中部,除沿金华江及主要支流乌义江等陆续有厚度小于10米的第四系松散层分布外,盆地内主要分布呈梳状丘岗的裸露红色碎屑岩。
Located in the central part of Zhejiang Province, the Jinhua Basin is part of the Jinqu Basin, the largest inland basin in Zhejiang. But in itself it is still a closed syncline basin. The southern and northern boundaries of the basin are mainly middle and low mountains formed by Upper Jurassic pyroclastic rocks. The east-west extension adjoins Shotang and Bailongqiao synclines. Jinhua River traverses the central part of the basin except for the distribution of Quaternary loose layers with a thickness of less than 10 meters along the Jinhua River and the major tributary of Wuyi River. There are mainly bare red clastic rocks with comb-shaped hillocks in the basin.