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℃/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。
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
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 。
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。
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。
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。
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 。
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。
The formation and accumulation of coalbed gas are closely related to the paleogeothermal field of the coal metamorphism.
煤层气的形成和赋存与煤变质的古地温场条件密切相关。
According to the principles of systematic, dynamic and comprehensive, the characteristics of tectonics and paleogeothermal field of Hefei basin are studied, by means of the combinative methods of geology, geophysics and multi-testing about vitrinite reflectance and apatile fission track.
以含油气盆地研究的整体、动态、综合原则为指导，运用盆地构造与区域构造研究相结合、盆地构造演化与古地温场分析相结合、地质与地球物理及多种测试手段相结合的综合研究方法，对中新生代合肥盆地的构造演化及古地温场特征进行了系统研究。
The optimal identification of parameters in three dimension paleo-geotemperature equation;
三维古地温度场方程的参数优化识别
STUDY OF PALEOTEMPERATURE OF THE LOWER CAMBRIAN BLACK SHALE SERIES AND THEIR IMPLICATIONS IN NORTHERN GUIZHOU PROVINCE
黔北下寒武统黑色岩系古地温及其指示意义
The Research on Relationship between Paleogeothermal Evolutional History and Various Mineral Deposits in Ordos Basin;
鄂尔多斯盆地古地温演化与多种能源矿产关系的研究
The key of computing palacseotherm by thermal conduction basic formula is the restoration palae-heat flow Q.
其思路是：古地温按热传导的基本公式进行计算，其中关键是古热流Q的恢复；
The maturity of the organic matters in this basin is mainlly controlled by the palaeo-geotemperature,the degree of tectonic deformation and pyrogenetic rock and plutonic hot fluid.
羌塘盆地有机质成熟度主要受古地温、构造变形程度和火成岩及深成热流的控制。
《Mongolian Secret History》 Tengger (Heaven)-Etugen (Earth)-Gu Wen (Human) Trinity Ethical Relationship Research;
《蒙古秘史》之腾格里（天）—额秃根（地）—古温（人）三位一体伦理关系研究
Reserch on Construction of Spa Tourism in Ethnic Regions Takeing an Example of Mongolia Style Spa Tourism in Inner Mongolia;
民族地区温泉旅游的建设研究——以内蒙古“蒙式温泉”旅游构建为例
Goodwin comes in and tells her to contact the local sheriff.
古德温进屋来叫她去与当地县长取得联系。
A DUCTILE SHEAR ZONE IN THE WENDUERMIAO AREA, NEI MONGGOL (INNER MONGOLIA)
内蒙古温都尔庙地区韧性剪切带的研究
Geological characteristics of Wengeng thrust fault in Langshan area of western Inner Mongolia
内蒙古西部狼山温更逆冲断层的地质特征
Geological Features of Gold(Copper, Molybdenum)Mineralization in Chaokewenduoer, Inner Mongolia
内蒙古朝克温多尔金(铜、钼)矿成矿地质特征
Analysis on Variation Characteristics of Temperature Abnormality and its Possible Impact in Inner Mongolia
内蒙古地区气温异常变化特征及可能影响分析
Seasonal and regional differences of air temperature changes in Inner Mongolia
内蒙古地区气温变化的季节和区域差异
Retrieval of land surface temperature of Inner Mongolia using MODIS image and split window algorithm
用MODIS数据和分裂窗算法反演内蒙古地区的地表温度
CURIE ISOTHERMAL SURFACE AND HEAT FLOW ANALYSIS OF THE ADJACENT REGION OF THE NIANQING TANGGULA PIEDMONT FAULTED ZONES
念青唐古拉山前断裂系周围地区的居里等温面与热流分析
The Quantified Estimate of the Temperature from the Late Pliocene to the Early Pleistocene in Nihewan Basin-Based on the Statistics of the Number of Species of Arviclinae;
利用Arvicolinae对泥河湾盆地晚上新世—早更新世古温度定量化研究
Analysis of Land Surface Temperature in Ancient City Area of Suzhou and Its Role on City Planning
苏州古城区地面温度分析及在城市规划中的作用
Quantifying the denudations of major tectonic events in Sichuan basin:Constrained by the paleothermal records
利用古温标恢复四川盆地主要构造运动时期的剥蚀量