鄂尔多斯盆地白垩系沉积建造对地下水的控制  

Controls of the Cretaceous sedimentary formations on the groundwater in the Ordos Basin

作　　者：谢从瑞[1] 杨忠智[2] 王永和[1] 谢渊[3] 

机构地区：[1]西安地质矿产研究所,陕西西安710054 [2]长安大学地球科学学院,四川西安710061 [3]成都地质矿产研究所,四川成都610081

出　　处：《沉积与特提斯地质》2013年第2期40-45,共6页Sedimentary Geology and Tethyan Geology

摘　　要：有关鄂尔多斯盆地地下水系统,前人已做过大量的研究,总结出不少的成果和规律。但从沉积建造方面研究地下水系统的不多。本文详细研究了白垩系沉积建造的特征和规律,探讨其对于研究区白垩系地下水系统的形成、富集和赋存的影响和控制,对于研究区白垩系地下水的开发和利用提供了重要的依据。Plentiful groundwater as one of the favourable natural resources in the development and construction is hosted in the Cretaceous strata in the Ordos Basin. Up to now, numerous studies have been conducted on these groundwater systems in the Basin. The present paper deals, in detail, with the effects and controls of the Cretaceous sedimentary formations on the generation, enrichment and preservation of the Cretaceous groundwater systems, and thus provides useful information for the development and utilization of the groundwater in the Ordos Basin.

关 键 词：鄂尔多斯盆地 白垩系 地下水 沉积建造 

分 类 号：P641.11[天文地球—地质矿产勘探]