geothermal gradient

The effects of the geothermal gradient and bottom water temperature are great .

由此可见，在这几种因素中，地温梯度和底水温度对稳定带厚度的影响较大。

The deeper the depth , the higher the geothermal gradient .

此外，地温随深度加大而增高。

Geothermal gradient and heat flow values of some deep wells in Sichuan Basin

四川盆地地温梯度及几个深井的热流值

Low temperature geothermal gradient utilization systems using serial mode of radiator and water source heat pump

散热器与水源热泵串联的低温地热梯级利用系统应用分析高频感应加热蒸镀设备

It has discussed the distributing disciplinarian and controlling factors of geothermal gradient .

计算了地温梯度，探讨了分布规律和控制因素。

The present geothermal gradient of the Huh Lake depression is3 .

呼和湖凹陷现今地温梯度为3。

And ③ having a geothermal gradient of 3.66 ℃ / m and surface temperature of 20 ℃ .

地温梯度为3.66℃／100m，地面温度20℃。

Modern hydrocarbon in all formations mainly accumulates where residual pressure is low and geothermal gradient is high .

现今各层系的油气主要聚集在剩余压力低值区和地温梯度高值区。

Have vertically , as the increase geothermal gradient of the depth has the tendency to reduce .

纵向上，随深度的增大地温梯度有减小的趋势。

The map of geothermal gradient of Cenozoic sedimentary cover in the North China Plain and its brief explanation

华北平原新生界盖层地温梯度图及其简要说明

The tunnel will get through zones of relatively low geothermal gradient and avoid zones of high earth temperature and high heat flow .

隧道避开了高地温和高大地热流的地段，经过区域的地温梯度相对较低。

Some Remarks about Geothermal Gradient of Sedimentary Basins

沉积盆地地温梯度研究中应注意的问题

Several distinctive characteristics of fluid dynamic field in Ying-Qiong Basin show high geothermal gradient , overpressure and intensive fluid activity .

莺&琼盆地具有高温、超压以及强烈的流体活动等独特的流体动力学特征。

The lower the geothermal gradient , the greater the formation pressure , formation of new era of Vietnam , diagenesis weaker .

地温梯度越低、地层压力越大、地层时代越新，成岩作用越弱。

Analyses the advantages of using low temperature geothermal gradient utilization system with serial mode of radiator and water source heat pump for retrofitted projects .

利用单位热成本的概念分析比较了几种供热方式的经济性，分析了散热器与水源热泵串联运行低温地热梯级利用供暖改造方案的优越性。

The current discovered large and medium oil and gas fields are concentrated on the low swell with high geothermal gradient in Liaoxi .

该地区目前已发现的大中型油气田多位于辽西低凸起高地温梯度区。

Submarine temperature , pressure , gas compositions , geothermal gradient and syngenetic water salinity control the depth of hydrate zone basement .

海底温度和压力、地热梯度、气体成分、同生水盐度等控制着水合物稳定带基底的深度和厚度。

Sedimentation / compaction , geothermal gradient , tectonic movements and deep fluid play a critical role in the formation of gas hydrate .

沉积压实、地温梯度、构造运动以及深部流体对水合物产生的效率起决定作用。

The paper constructs a correlation formula for the pressure gradient and geothermal gradient in the lithosphere with the thermocompression coefficient .

与地温梯度一样，岩石圈中的地压梯度在空间和时间上也应是复杂多变的。

Conclusion The maturity of resource rock is controlled by the paleo - thermal field and is independent of the geothermal gradient of nowadays .

结论烃源岩成熟度主要受古地温场的控制，而与现今地温梯度无关；

The result shows that average geothermal gradient of this area is 40.8 ~ 41.3 ℃ / km , which is higher than that of nowadays .

结果表明，该区平均古地温梯度为40·8~41·3℃/km，高于现今平均地温梯度。

The results indicate that ( 1 ) The average present geothermal gradient is 35.8 ℃ / km , showing a decreasing trend with depth ;

结果表明：（1）现今地温梯度为35.8℃/km。

The west part of China has been in the crust compression and thickening background , geothermal gradient and heat flow are lower in the basins .

而西部处于地壳挤压增厚构造背景，沉积盆地地温梯度及大地热流值较低。

Sine Cenozoic , the eastern region of China has been in stretching background , geothermal gradient and heat flow are high in the basins ;

新生代以来中国东部处于拉张背景，沉积盆地地温梯度及大地热流值高；

A compilation of geothermal gradient map was obtained by using some related data of geothermal gradient and the Curie isothermal surfaces were calculated .

利用地温梯度资料，编制了甘宁青地区地温梯度分布图，估算了居里温度面。

In the Carboniferous to Permian period , geothermal gradient increased , and could be up to 3 ~ 3.2 ℃ / 100 m.

石炭&二叠纪古地温略有上升，地温梯度可能达到3～3.2℃/100m；

The high value of thermal current and the high geothermal gradient indicated that the Qiongzhou strait is an active rift stucture in recent year .

该地区的高热流值、高地热增温率和强震活动都说明，琼州海峡是现今仍具有一定活动性的裂谷构造。

It decreases about 660m when the geothermal gradient changes from 0.02 ℃ / m to 0.1 ℃ / m.

水深2000m情况下，地温梯度从0.02℃/m到0.1℃/m变化时，稳定带厚度减薄了大约660m；

Temperature pattern shows that the highest temperature and geothermal gradient appears in the central part of the Field , which is the discharge area of the Zhangzhou Basin .

温度场研究表明，热田中心区具有最高温度和最大的地温梯度，此乃漳州盆地的排泄区。

Paleo geothermal gradient was higher than that at the present . The study estimated that denudation thickness of the area was more than 2000 meters .

古地温梯度比现地温梯度低，估计本区整个剥蚀厚度大于2000m。