甘肃疏勒河断裂中段核废物处置库稳定性研究  

STUDY ON STABILITY OF HLW RESPOSITORY IN THE MIDLE REGION OF SHULE RIVER FAULT ZONE

作　　者：余运祥[1] 刘林清[1] 莫撼[1] 

机构地区：[1]华东地质学院地球科学系

出　　处：《华东地质学院学报》1995年第3期243-248,共6页Journal of East China Geological Institute

摘　　要：本文利用遥感图像解译、地质调研和物探等技术手段，对甘肃疏勒河断裂带中段的地质特征及其稳定性进行了研究。通过研究，对疏勒河断裂带的认识有了新的进展，取得了较好的效果。第一，在人工露头上观察到疏勒河断裂带中段主干断裂的结构面特征，初步确定其力学性质以压性为主；第二，在该区开展甚低频电磁测量，其成果与遥感图像解译、地质调研的结果一致，从而肯定了疏勒河断裂带中段空间分布规律的认识；第三，应用区域地球物理和地球地温资料，对疏勒河断裂带的深部地壳结构和地温背景进行了分析研究，获得了一些深部地质信息。同时，对勒勒河断裂带中段的稳定性进行了评述，并指出该断裂带中段及其以北的北山地区较稳定，是高放废物处置库选址的有利地区。The paper studies the geological features and stability of the middle region of shule riverfault zone by means of the interpretation of remote sensing images,geological researches and geophysi-cal prospecting.The knowledge of shule river fault zone is much improved.The structural plane fea-tures of the trunk fault of the middle region of shule river fault zone are observed at hand-outcrop ,andits mechanics character is preliminary determined as compression.The result of VLF electromagneticmeasurement on this area is consistent with the result of the interpretation of remote sensing images,and geological researches.It is confirmed that the Knowledge of the space distribution law of the middleregion of sh ule river zone.Some deep geological in formation is obtained from analysing and studyingdeep crust structure and earth temperature background by use of the regional geophysical and earthtemperature date.The comment on stability of the middle region of the shule river fault zone indicatesthat its middle region and the north mountain which is located the north of shule river fault zone havebetter stability.It is perfect area for being the site of HLW respeitory.

关 键 词：核废物处置库 稳定性 疏勒河 断裂 

分 类 号：TL942.211[核科学技术—辐射防护及环境保护]