检索规则说明:AND代表“并且”;OR代表“或者”;NOT代表“不包含”;(注意必须大写,运算符两边需空一格)
检 索 范 例 :范例一: (K=图书馆学 OR K=情报学) AND A=范并思 范例二:J=计算机应用与软件 AND (U=C++ OR U=Basic) NOT M=Visual
机构地区:[1]中国地质大学地球物理与信息技术学院,北京100083 [2]中国地质科学院地球物理地球化学勘查研究所,河北廊坊065000
出 处:《物探与化探》2011年第3期325-328,共4页Geophysical and Geochemical Exploration
摘 要:在利用电阻率参数进行地热田勘查时,将电阻率参数转换为温度参数后形成的温度断面图能够更直观地显示地下温度场的分布情况;当勘查剖面有已知地热钻孔时,能够利用已知钻孔温度预测地下温度场的温度分布,这对判定热储构造分布、确定钻孔位置十分有利。温度计算时,地层电阻率初值的计算和勘查方法有关,选择正确的电阻率初值计算方法对温度计算结果至关重要。笔者对电阻率计算温度方法、地层电阻率初值计算方法进行了探讨,这对地热田勘查解释具有重要意义。When the resistivity of the parameters is used in geothermal field exploration,the temperature sectional drawing made by the conversion of resistivity parameters to temperature paremeters is a more intuitive graph to show the distribution of underground temperature.When known geothermal drilling is available in the exploration profile,it is possible to use the known temperature drilling to forecast field distribution of the underground temperature,and this is advantageous to determining the distribution of thermal energy storage structure and the position of the drill hole.In temperature calculation,the calculation of initial formation resistivity is related to the surveying method.The choice of the correct calculation of initial resistivity is very important for temperature calculation results.This paper deals with the calculation method for temperature based on resistivity and initial resistivity value of strata,which is important in explaining the geothermal field exploration.
关 键 词:地热田 温度预测 热储构造 电阻率-温度计算方法
分 类 号:P631[天文地球—地质矿产勘探]
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在链接到云南高校图书馆文献保障联盟下载...
云南高校图书馆联盟文献共享服务平台 版权所有©
您的IP:216.73.216.147