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矿泉水位于市西20公里,属吴县光福乡,往西有水路可通太湖,往东有公路可通苏洲(见图1)。当地的地形地貌,属低山丘陵景观,玉屏山山顶高程192米,周围平地高程13米,附近有城隍山、五龙山、石塘山、正山、借尼山等。高程均在100—200米,在玉屏山以南约3公里为穹窿山,山顶高程342米,为附近最高峰,区域构造,属下扬子拗陷太湖隆起,苏州—湖州断块的东缘,出露地层,除城隍山、石塘山为石英斑岩,借尼山为页岩外,余玉屏山、五龙山、正山、穹窿山均为泥盆系茅山群砂岩和五通组砂岩所分布,裂隙发育,断
Mineral water is located 20 kilometers west of the city, is Wuxu Guangfu Township, west of the waterway through the Taihu Lake, east of the road through Suzhou (see Figure 1). Local topography, is a hilly landscape, elevation of 192 meters Yuping Mountain, the surrounding elevation of 13 meters, near the Chenghuang Mountain, Wulong Mountain, Shitangshan, are mountains, by Nishan and so on. Elevation of 100-200 meters, about 3 kilometers south of Yuping Mountain Dome Hill, the peak elevation of 342 meters for the nearby peak, the regional structure, the Yangtze subduction of the Taihu uplift, the eastern edge of the Suzhou - Huzhou fault block, Exposed to the strata, except for the Chenghuang Mountain, Shitang Mountain, quartz porphyry and Niushan Shale, the Yuyuping Mountain, Wulong Mountain, Zhengshan Mountain and Qionglong Mountain are both the Devonian Mingshan Group Sandstone and the Wutong Formation Sandstone Distribution, fracture development, broken