山西(交城)花岗岩体地质环境与理化特征研究  

Geologic setting and Physical chemical characteristics of Jiaocheng Granite of Shanxi

作　　者：李春江[1] 李书绅[2] 陈式[2] 周子荣[2] 

机构地区：[1]中国农业大学 [2]中国辐射防护研究院

出　　处：《水文地质工程地质》1998年第4期46-49,共4页Hydrogeology & Engineering Geology

基　　金：核工业科学基金

摘　　要：本论文对交城花岗岩体的地质环境、工程力学和理化特征作了初步研究。认为交城花岗岩体的地质构造稳定、水文地质条件良好，岩性均匀，故选择交城花岗岩作为研究主岩，并对典型核素在填隙物和花岗岩上的吸附性能进行了试验。This paper studies primarily the geologic setting, engineering geology, and physical chemical characteristic of the Jiaocheng granite. Results show that geological structure is stable, hydrogeological condition is good, and the lithology is uniform. The granite of Shanxi is choiced as the host and the adsorption function of typical nuclides to fissure fillings and granite is tested.

关 键 词：花岗岩体 高放废物 地质处理 理化特征 地质环境 

分 类 号：P588.121[天文地球—岩石学] TL942.1[天文地球—地质学]