1) ancient Wen state
古温国
1.
A distinction between ancient Wen state and ancient Su state is imperative in studying the territory and boundary of ancient Su state.
研究古苏国地理及其疆域 ,应区别古温国与古苏国。
2) Ancient cities and countries
古城古国
3) ancient state
古国
1.
The appearance of settlements and settlement clusters in Yangshao culture were earlier than the other cultures The prehistoric settlement clusters developed from tribes to ancient states Yangshao culture is in the core position in all Neolithic cultures of Chin
史前聚落群先是高级阶段的部落 ,后是古国 ,经历了从部落到国家的发展过程。
4) 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。
5) 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。
6) 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 。
补充资料：灵幽（唐上都大温国寺）《宋高僧传》卷第二十五
【灵幽（唐上都大温国寺）《宋高僧传》卷第二十五】
释灵幽。不知何许人也。僻静淳直诵习惟勤偶疾暴终。杳归冥府引之见王问修何业。答曰。贫道素持金刚般若。已有年矣。王合掌屡称善哉。俾令讽诵。幽吮唇播舌章段分明念毕。王曰。未尽善矣。何耶。勘少一节文。何贯华之线断乎。师寿命虽尽。且放还人间十年。要劝一切人受持斯典。如其真本即在濠州钟离寺石碑上。如是已经七日而苏。幽遂奏奉敕令写此经真本。添其句读。在无法可说是名说法之后是也。
［赞宁］系曰。春秋夏五不敢轻加。佛教宜然无妄酿矣。通曰。灵幽获钟离寺石经。符合无苦。如道明所添糅。使人疑豫。必招诈伪。率易改张称有冥告。诫之哉。
释灵幽。不知何许人也。僻静淳直诵习惟勤偶疾暴终。杳归冥府引之见王问修何业。答曰。贫道素持金刚般若。已有年矣。王合掌屡称善哉。俾令讽诵。幽吮唇播舌章段分明念毕。王曰。未尽善矣。何耶。勘少一节文。何贯华之线断乎。师寿命虽尽。且放还人间十年。要劝一切人受持斯典。如其真本即在濠州钟离寺石碑上。如是已经七日而苏。幽遂奏奉敕令写此经真本。添其句读。在无法可说是名说法之后是也。
［赞宁］系曰。春秋夏五不敢轻加。佛教宜然无妄酿矣。通曰。灵幽获钟离寺石经。符合无苦。如道明所添糅。使人疑豫。必招诈伪。率易改张称有冥告。诫之哉。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
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