摘要
The weathering crevices and tectonic crevices are developed well in Panshan granite.The crevices direction is NE45°-65°and NW310°-340°. Ground water is stored in all kinds of the granite crevices and getes elements from rock.The common elements of the granite crevice-water in Panshan are K<sup>+</sup>, Na<sup>+</sup> , Ca<sup>2+</sup>, Mg<sup>2+</sup>, CI<sup>-</sup>, SO<sub>4</sub><sup>2-</sup>, HCO<sub>3</sub><sup>-</sup>, SiO<sub>2</sub> ect. and the trace elements are Sr<sup>2+</sup>, Li<sup>+</sup>, F<sup>-</sup>ect..Their average content is showed in table 1. Specially in the fault tectonic,the type of water chemistry is H. S-N which is different from other and the contains of trace element Li<sup>+</sup> , Sr<sup>2+</sup> , F<sup>-</sup> is higher.
出处
《石家庄经济学院学报》
1995年第S1期80-81,共2页
Journal of Shijiazhuang University of Economics