论花岗岩与凝灰熔岩地质交界区勘察方式与方法  

Exploration Methods and Methods for the Geological Junction Area of Light Granite and Tuff Lava

作　　者：连爱联 Lian Ailian(Fujian Panji Geotechnical Engineering Co.,Ltd.,Xiamen,Fujian 361000)

机构地区：[1]福建磐基岩土工程有限公司

出　　处：《江西建材》2019年第12期56-57,共2页Jiangxi Building Materials

摘　　要：以工程实际为例,通过分析花岗岩与凝灰熔岩地质交界区基岩埋深变化大、裂隙水自冒、风化不均匀等危害原因,提出了一些具体的勘察方式与方法。Taking the engineering practice as an example, through analyzing the dangerous reasons such as the great change of the buried depth of the bedrock in the geological junction area of granite and tuff lava, the self emergence of fissure water, and the uneven weathering, some specific exploration methods and methods are put forward.

关 键 词：花岗岩 不均匀 基岩裂隙 勘察方法 

分 类 号：TU195[建筑科学—建筑理论]