论文部分内容阅读
内蒙古自治区地处我国北部,地域广阔,区域内构造、地形、地貌类型多样,地表水、地下水及矿泉水资源较为丰富。区内矿泉水资源多分布于活动构造断裂带和岩浆活动区及沉降盆地区。内蒙古自治区天然饮用矿泉水大致包括岩浆活动型、构造断裂型、沉降盆地型三类地质构造成因类型。全区天然饮用矿泉水资源按照赋存、出露地质条件可分为:带状出露型、带状埋藏型、带—层状埋藏型、层状埋藏型4种类型。常见的矿物类型为:锶型、偏硅酸型、锶硅或硅锶复合型。
Inner Mongolia Autonomous Region is located in the northern part of our country. It has a vast territory, diverse structures, terrain and topography within the region. There are abundant surface water, groundwater and mineral water resources. The mineral resources in the area are mainly distributed in the active tectonic fault zone, the magmatic activity zone and the sedimentation basin. Natural drinking mineral water in Inner Mongolia roughly includes three types of geological tectonic types: magmatic activity type, tectonic fracture type and subsidence basin type. The region’s natural drinking mineral water resources in accordance with occurrence, exposure to geological conditions can be divided into: banded exposed, belt buried, belt - layered buried, buried buried four types. Common types of minerals: strontium, metasilicate, strontium silicon or silicon-strontium composite.