岩石热导率

中国东南地区岩石热导率值的分析

Analysis on the thermal conductivity of rocks from SE China

指出地温梯度的变化在纵向上大致可划分为四段，这主要是由于岩石热导率的差异而造成的；

They are mainly caused by the difference of thermal conductivity of rocks .

以Ungerer等提供的岩石热导率与岩性、地温之间的关系曲线为基础，采用双重回归方法建立了岩石热导率的经验公式。

And ( 3 ) Based on the relation curve among thermal conductivity , lithologic characters and earth temperature provided by Ungerer etc , the authors establish an empirical formula about the thermal conductivity of rock through double regression .

含油气盆地中热传导与岩石热导率研究

Petroliferous basin in the rock thermal conductivity and thermal conductivity research

岩石热导率的温压实验及分析

An experimental study of rock thermal conductivity under different temperature and pressure

孔隙岩石热导率的饱水试验研究

Experimental research on the thermal conductivity of water-saturated porous rocks

岩石热导率与声波速度的相关分析

Correlation between thermal conductivity and acoustic velocity of rocks

地热Ⅱ型稳定分棒式热导仪岩石热导率精密测量装置

Geotherm - ⅱ model thermal conductivity meter of steady-state divided bar type & a precise rock thermal conductivity measuring device

通过对鄂尔多斯盆地地壳结构、岩石热导率和生热率的综合研究，盆地莫霍面现今平均温度为568.5℃。

According to the experimentation of heat generation , heat conductivity , etc. , the Ordos basin is characterizing of its average temperature of Moho 568.5 ℃ .

19851986年度和19861987年度在菲尔德斯半岛对地面温度进行了测量，共获得129个数据，并对带回的样品进行了岩石热导率测量，共获得210个数据。

During 1985-1986 and 1986-1987 expeditions on Fildes Peninsula the ground temperature in 119 spots was measured . Then thermal conductivity measurements were made on the rock samples collected .

本文根据大量实测数据，首次系统地报道了中国西北地区塔里木盆地、准噶尔盆地和柴达木盆地内的岩石热导率、岩石放射性生热率数据及其分布特征。

The characteristics of thermal conductivity and radiogenic heat production rate of rocks in the Tarim , Junggar and Qaidam Basins , Northwest China , were analysed systematically based on a large amount of measured data .

利用超高压变质岩的P波速度估算地下岩石的热导率

Prediction of Thermal Conductivity of Underground Rocks from P-Wave Velocity of Ultrahigh-Pressure Metamorphic Rocks

砂岩和泥岩的平均热导率值分别为3.41±1.22W／m.K和3.59±1.19w／m.K，而且在区域上同类岩石的热导率值变化幅度很大。

The mean value of sandstone and mudstone from SE China appears to be 3 . 41 ± 1 . 22W / m. K and 3 . 59 ± 1 . 19w / m. K respectively and it varies in a wide range .

岩石的热导率对岩石热变质的影响

Influence of thermal conductivities on thermal metamorphism of wall rocks

通过对面理发育的样品进行测试，东海地区各类岩石的热导率具有较明显的各向异性。

The anisotropy of thermal conductivity and its possible influencing factors are discussed for the rocks in Donghai area .

研究结果表明，这些岩石的热导率值主要受控于其矿物成分，特别是石英的含量。

Studies demonstrate that the thermal conductivity of these rocks is mainly controlled by the contents of minerals , especially by the quartz content .

粉砂岩的热导率基本介于泥岩和砂岩之间。岩石的热导率和岩石样品所处的深度密切相关，随着深度的增大热导率数值增大。高含水期粉砂岩储层水淹层解释方法研究

The thermal conductivity is varied with depth , it usually become higher with depth . Water-out Reservoir Interpretation Method in Siltstone Reservoirs at High Watercut Stage

利用四川东北地区现有的钻井测温数据及测定的岩石样品热导率数据，计算了12口钻井的大地热流值。

Based on available borehole temperature logging and thermal conductivity measurement of core samples in the northeastern Sichuan Basin , we have estimated 12 terrestrial heat flow values .

本文根据热田内152个钻孔的测温资料和56块岩石样品的热导率数据，采用三种不同方法计算出漳州热田及其邻近地区的大地热流值，并讨论了热流值分布的特点。

Based on 152 temperature measurements in boreholes and thermal conductivity determinations on 56 rock samples , heat flow values in different parts of the Field have been calculated by using 3 different approaches . The characteristics of heat flow distribution in Zhangzhou Geothermal Field were discussed in this paper .

利用地表大地热流观测资料、岩石生热率及热导率数据研究了三江和四川盆地6个地区的岩石层平均温度结构及强度分布。

The averaged lithospheric thermal and strength structure of six tectonic units in Sanjiang region and Sichuan Basin is investigated by using the surface heat flow data , rock heat generation rate and thermal conductivity .