1) paleogeotherm
古地温曲线
1.
Geothermobarometry is a fundamental way for constructing a paleogeotherm.
古地温曲线是岩石圈在特定地质时期热结构的集中体现。
2) geothermal curve
地温曲线
1.
Based on the study of the mineral dehydration and the geothermal curves of typical areas and the phase diagram of water and the water contents of some mineral and rocks,the paper shows that water is liquid or vapor respectively above or under 15.
在对水的相图、典型地区的地温曲线、矿物的脱水行为及一些矿物和岩石的含水量等研究的基础上指出 ,以 15 。
3) palaeotemperature
古地温
1.
The palaeotemperature evolution of Bayindulan depresion has been recovered with the method of vitrinite reflectance.
应用镜质体反射率法恢复了巴音都兰凹陷的古地温演化史，研究结果表明巴音都兰凹陷侏罗纪与白垩纪具有不同的地温场特征，晚侏罗世古地温梯度高于早白垩世地温梯度，早白垩世地温梯度可达4。
2.
2℃/100m between Tertiary and Quaternary period because of the continuous uplift erosion and the decrease of the Terrestrial heat flow, which made the palaeotemperature begin to decrease at early Tertiary.
8℃/100m,古地温比现今温度更高。
4) palaeogeotherm
古地温
1.
Studying the palaeogeotherm of Dongying Sag by using vitrinite reflectance;
应用镜质体反射率方法研究东营凹陷古地温
2.
This paper restores the palaeogeotherm and palaeogeothermal gradient in Songliao Basin using several methods.
通过多种古地温研究方法恢复了松辽盆地的古地温及古地温梯度 ,研究结果表明松辽盆地古地温高于今地温 ,白垩纪末的地温梯度及大地热流值可达 4 2 6～ 4 80℃ 10 0m和 95～ 10 7mW m2 ,远高于现今地温梯度 3 70℃ 10 0m及大地热流值 69mW m2 。
3.
There were two relatively high palaeogeothermal stages,one in Cambrian-Early Ordovician and the other in Carboniferous-Permian.
塔里木盆地自古生代以来古地温总体呈下降趋势,其间存在两个相对较高的古地温期:一个是寒武纪—早奥陶世,另一个是石炭—二叠纪。
5) paleotemperature
[,pæliəu'tempərətʃə]
古地温
1.
Fluid inclusion microthermometry and apatite fission track analysis were used to reconstruct the Tertiary paleotemperature of the East depression,Liaohe basin.
以太阳岛构造和大平房构造为例,利用流体包裹体显微测温和磷灰石裂变径迹分析方法恢复了辽河盆地东部凹陷第三系的古地温。
2.
The present temperature has been studied with testing data and the paleotemperature has been restored with fission track in apatite and fluid inclusion in Damingtun sag.
利用系统测温资料和试油资料研究了大民屯凹陷现今地温特征 ,利用磷灰石裂变径迹、流体包裹体均一温度恢复了古地温 ,利用EasyRo模型反演热史变化 ,并与东西部凹陷热史进行了对比。
3.
Based on the experiment, this research calculates kinetic parameters of kerogen vitrinite reflectance (R_o) through KINETICS software, and then calculates Cambrian-Ordovician paleotemperature of the well Tacan 1 combined with burial history.
通过热解动力学模拟实验 ,对塔里木盆地塔参 1井奥陶系干酪根的热演化过程进行了模拟 ,在此基础上利用KINETICS软件求取干酪根镜质体反射率 (Ro)的生成动力学参数 ,并结合塔参 1井的沉积埋藏史 ,计算塔参 1井寒武—奥陶系的古地温 ,这对于研究塔里木盆地下古生界高过成熟烃源岩的古地温是一种新方法 。
6) paleo-temperature
古地温
1.
The research results on the temperatures determined from the fluid inclusions showed that the paleo-temperature experienced three periods change, which was corresponding to that of the migration and accumulation of oil-gas.
依据流体包裹体测温学研究,本区的油气形成过程主要经历了三期古地温变化,并与油气运移和成藏期次相一致。
补充资料：Hesse曲线(代数曲线的)
Hesse曲线(代数曲线的)
Hessian (algebraic curve)
11油限曲线(代数曲线的)【H台自11(.妙如允.抖e);recc咖，T~aaa，即r药pa一吸ee二o‘二p.助蓝] n次代数曲线(司罗玩水c~)的He丈祀曲线就是其极二次曲线能分裂为两条直线的点的集合，也是第一极曲线的二重点构成的集合.n次非奇异曲线的He丈七曲线是一条次数为3伪一2)、类为3(n一2)(3n一7)的曲线.设介O是这条n次曲线的齐次坐标方程，关丘=刁:f/刁xi刁、，则它的He丈犯曲线的定义方程为 !不:关:五，} }五:关:五31=0. }人，人2人3}特征不等于3时的三次非奇异曲线的H既七曲线与这条曲线交于9个通常拐点.因O.H改e(l 844)而得名. A .E.H困阳。B撰
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条