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geothermal history     
相关语句
  地热史
     The study of buried history,geothermal history,source-reservoir-seal assemblage and hydrocarbon-expulsion history of the depression showed that the pools generated by the coal-related source rocks in the Upper Paleozoic were formed in two stages of the Late Mesozoic and the Palaeogene periods to present.
     对黄骅坳陷孔西潜山埋藏史、地热史、生储盖发育史和排烃史的研究表明,上古生界煤系烃源岩主要形成两期油气藏,第一期油气成藏发生在晚侏罗世—早白垩世,该期生烃量有限,成藏规模较小;
短句来源
     RECONSTRUCTION OF GEOTHERMAL HISTORY IN HYDROCARBON BASINS
     油气盆地地热史恢复方法
短句来源
     STUDY ON GEOTHERMAL HISTORY IN SWELL AREA OF SOUTHEAST SONGLIAO BASIN BY USING SEVERAL PALEOGEOTHERMOMETERS
     利用多种古地温计研究松辽盆地东南隆起区的地热史
短句来源
     Abstract On the basis of vitrinite reflectance, K-Ar ages and apatite fission-track data,the time of hydrocarbon generation and migration, migration direction and hydrocarbon exploration direction are discussed starting with the reconstruction of the subsidence and uplift history and geothermal history of the Ordos Basin.
     本文根据镜质体反射率、K-Ar年龄和磷灰石裂变径速资料,从恢复鄂尔多斯盆地的沉降抬升史与地热史入手,讨论了油气形成与运移的时间、运移方向及其油气勘探方向。
短句来源
     INFLUENCE OF RADIOACTIVE HEAT GENERATION WITHIN LITHOSPHERE ON GEOTHERMAL HISTORY OF EXTENSIONAL BASIN
     岩石圈生热效应对拉张盆地地热史的影响
短句来源
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  热史
     Integrated with the geothermal history and burial history,the formation time of inclusions is about 120 Ma,85 Ma and 72 Ma,respectively.
     与热史和埋藏史相结合,推测油气藏的成藏时间约为120 Ma前,85 Ma前和72 Ma前左右。
短句来源
     Geothermal History Simulation of Sediment Basins Under Dynamic Coupling on the Pressure and Temperature Field
     温度场与压力场动态耦合下的沉积盆地热史模拟
短句来源
     Study of geothermal history in Qingnan sub-sag with the Easy-R o(%) numerical modeling software shows that the Cretaceous and Tertiary palaeo-geothermal gradients are 30℃/km and 29℃/km,respectively.
     应用Easy Ro(% )数值模拟软件对青南次凹地热史的研究表明 ,白垩纪与第三纪的古地温梯度分别为 30℃ /km和 2 9℃ /km。
短句来源
     BAS1 system is based on some advanced models published already and other advanced models written by ourselves,and consists of four models:Geohistory, Geothermal history,Hydrocarbon-generation history,and Kydrocarbon-expulsion history.
     BAS1系统是在既吸收国际上某些先进模型、又独创一些模型的基础上建成的,包括四个模型:地史,热史,生烃史,排烃史。
短句来源
     The model includes five model blocks:burial history,geothermal history,maturity history,hydrocarbon generation history and hydrocarbon expulsion history.
     该模型包括埋藏史模块、热史模块、成熟史模块、生烃史模块与排烃史模块5个组成部分,模块之间具有密切的联系,前一模块的输出结果可作为后一模块的输入条件。
短句来源
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  热历史
     Based on heat flow measurements and vitrinite reflectance ( R o) data, the geothermal history of Eastern Depression of the Liaohe Basin was reconstructed, which indicated that the Eastern Depression was characterized by lower present day heat flow varying between 47~70 mW/m 2, and that the depression experienced a much higher heat flow (66~82 mW/m 2) period from 43 Ma to about 25 Ma ago.
     根据辽河盆地东部凹陷大地热流测量和镜质体反射率数据 ,恢复了该区的热历史 ,结果表明 :东部凹陷热流呈现古热流高现今热流低的变化特征 ,沙河街组三段沉积期到东营组沉积期 (距今 43~ 2 5Ma)盆地热流为 66~ 82mW m2 ,现今热流值为 47~ 70mW m2 。
短句来源
     As the structural development and evolution histories are different in various structural units,the geothermal history of each structural unit in Tarim basin has distinct characteristics.
     由于盆地不同构造单元构造发展演化史不同,塔里木盆地各构造单元的地质热历史各具特征。
短句来源
     Mainly based on the study of fission track of the apatites, as well as geochronology, stable isotope composition and inclusion analysis, the principle and method of studying the geothermal history of sedimentary basin have been expounded systematically, and the source of sedimental materials, and the geotHermal characteristics of five section areas in Liaohe Basin.
     以磷灰石裂变径迹特征研究为主,辅以同位素地质年代学、稳定同位素组成及包体研究,系统阐明了研究沉积盆地热历史的基本原理和方法,确定了辽河盆地沉积地层物质来源及五条剖面的热历史特征。
短句来源
     Mainly based on the study of fission track of the apatites, as well as geochronology, stable isotope composition and inclusion analysis, the principle and method of studying the geothermal history of sedimentary basin have been expounded systematically, and the source of sedimental materials, and the geothermal characteristics of five section areas in Liaohe Basin were determined.
     以磷灰石裂变径迹特征研究为主,辅以同位素地质年代学、稳定同位素组成及包体研究,系统阐明了研究沉积盆地热历史的基本原理和方法,确定了辽河盆地沉积地层物质来源及五条剖面的热历史特征。
短句来源
     Geothermal history of Tarim basin is closely related with its structural evolution history.
     塔里木盆地的地质热历史与其构造演化史密切相关。
短句来源
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  地温史
     3. The hydrocarbon-generating history of source rocks from the Dongying Depression has been simulated by the Kinetics software, with the combination of burial and geothermal history.
     3.应用所获取的生烃动力学参数与Kinetics软件,结合牛庄洼陷地温史与埋藏史,对该凹陷代表钻孔进行了逼近地质条件下成烃规律模拟。
短句来源
     A 1-D MODEL FOR GEOTHERMAL HISTORY AND MATURATION OF ORGANIC MATTER
     地温史和有机质成熟史的一维模型
短句来源
     Therefore, the author presents a practical TTI R o method, the process of which is to firstly calculate the TTI history on the basis of the burial history from geohistory model and the temperature history from geothermal history model, and then to construct the R o TTI formulas for each geological period according to the field measured R o and TTI at the maximum burial depth of each formation, and finally to work out the R o history that is the hydrocarbon maturity history.
     提出实地TTI Ro法 :首先根据地史模拟得到的埋藏史以及热史模拟得到的地温史求得TTI史 ,再根据实测的Ro以及各地层埋深最大时的TTI值 ,制作各地质时期的TTI Ro公式 ,此后便可求得烃类成熟度史。
短句来源

 

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      geothermal history
    Maturation of source rocks will be greater for any given geothermal history if exhumation is incorporated in maturation modelling.
          
    Since calculation of the overpressure history uses the geohistory model and geothermal history model simulation outcomes, the relevant data used and the output of the two models of the Kela2 well are given as examples.
          
    Garnet in metapelites from the W?lz Complex of the Austroalpine crystalline basement east of the Tauern Window characteristically consists of two growth phases, which preserve a comprehensive record of the geothermal history during polymetamorphism.
          
    Considerable attention has been paid in recent years to the study of geothermal history by using spontaneous fission tracks of238U recorded in minerals.
          
    New progresses on geothermal history of Turpan-Hami Basin, Xinjiang, China
          
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    The core samples were collected from three oil-prospecting wells in Dongpu Depression of North China Basin and various parameters of fission track of apatite wells systematically measurad. The results show that the fission track zone of apatite in Dongpu Depression appears in the well interval from 1700 to 3300 m. Thus, the paleogeothermal gradient of different strata formed since Eogene in this region is obtained. To determine the ancient tectonic heat flow value in Dongpu Depression, 360 core samples have...

    The core samples were collected from three oil-prospecting wells in Dongpu Depression of North China Basin and various parameters of fission track of apatite wells systematically measurad. The results show that the fission track zone of apatite in Dongpu Depression appears in the well interval from 1700 to 3300 m. Thus, the paleogeothermal gradient of different strata formed since Eogene in this region is obtained. To determine the ancient tectonic heat flow value in Dongpu Depression, 360 core samples have been gathered from 21 prospecting wells in the region, and systematic measurements of rock heat conductivity have been done. With substitution of the rock heat conductivity in the formula, the ancient tectonic heat flow value of this region is yieled. On the basis of paleogeothermal parameters, the geothermal history of Dongpu Depression of North China Basin has been revealed and the geothermal maps of Eogene have been made.

    本文根据东濮凹陷文留地区的三口探井取得的13块岩芯,系统地做了磷灰石裂变径迹的测试。确定文留地区的磷灰石径迹衰退带的上限为2,000m,下限为3,500m。其温度范围为70℃~125℃。通过换算得到该区的古地温梯度,并取得区域的平均古大地热流值。根据测试资料,编制了径迹长度频谱图、绝对年龄与深度关系图。这些基础图对区域的古地温场的解释提供了较可靠的依据。

    1-Ditnensional Basin Simulator BAS1 has been created onmicrocomputer and IBM 4381 computer, and has been successfully applied to resource estimates of the eastern Lingqing Depression. BASl system consists of four models of geohistory, geothermal history, hydrocarbon-generation history and hydrocarbon-expulsion history. Input data include the information mainly from geology, well logging, seismology and geochemistry. The output results are the depositional history, structural history,paleo-heatflow...

    1-Ditnensional Basin Simulator BAS1 has been created onmicrocomputer and IBM 4381 computer, and has been successfully applied to resource estimates of the eastern Lingqing Depression. BASl system consists of four models of geohistory, geothermal history, hydrocarbon-generation history and hydrocarbon-expulsion history. Input data include the information mainly from geology, well logging, seismology and geochemistry. The output results are the depositional history, structural history,paleo-heatflow history, paleo-temperature history, R0 history, TTI history, hydrocarbon-generation history and hydrocarbon expulsion history in basin. The application of BASl in Lingqing depression is presented.

    在微机、IBM4381机和VAX8700机上研制成功了一维盆地模拟系统BAS1,并成功地用于临清坳陷东部的资源评价。BAS1系统是在吸收国际某些先进模型的基础上建立的一种新型系统,包括地史、热史、生烃史、排烃史四个模型。输入资料主要来自于地质、测井、地震和地化。输出结果是盆地的沉积史、构造史、古热流史、古地温史、TTI史、R_o史、生烃史和排烃史。本文介绍了应用BAS1系统揭示临清坳陷东部的石油地质特征。研究表明,该地区有勘探价值。

    The major source beds in the oil— bearing basins of Xinjiang are Paleozoic formations, therefore, it is rather important to study the paleogeothermal regimes of the basins.For the further study of the geothermal histories of the basins, the method of fission scar tracks in apatite is adopted, which suggests that the annealing temperatures (70~125℃) of fission tracks in apatite are within the temperature range (60~110℃) of substantial oil generation. Besides, the method is also used for solving the thermal history...

    The major source beds in the oil— bearing basins of Xinjiang are Paleozoic formations, therefore, it is rather important to study the paleogeothermal regimes of the basins.For the further study of the geothermal histories of the basins, the method of fission scar tracks in apatite is adopted, which suggests that the annealing temperatures (70~125℃) of fission tracks in apatite are within the temperature range (60~110℃) of substantial oil generation. Besides, the method is also used for solving the thermal history and some basic geological problems of sedimentary basins. The age of fission tracks represents the geological age of uplifting and erosion, s(?) it can be used for the timing of uplifting and erosion. The authors suppose a method of reconstructing geothermal history using enclosure temperature.The geothermal evolution of the Junggar Basin is divided into three major phases: a) the geosynclinal phase (Carboniferous Period) with paleothermal gradients, of 8~5 C/100m, b) the foredeep phase (Permian to the end of Triassic Period) with paleothermal gradients of 5~3℃ 100 m, and c) the platform phase (Jurassic to Paleogene) with paleothermal gradient of 3~2℃ 100 m. The Carboniferous and Permian source beds in a few major depressions of the basin reached the oil generation peak stage during Permian and Triassic Periods,therefore, the authors suggest that emphasis should be placed on finding Cenozoic reservoirs coupled with Paleozoic source beds.

    新疆含油气盆地的主要生油层是古生界,研究盆地的古地温显得尤为重要。 为进一步研究盆地的热史,引进了裂变径迹法,即磷灰石裂变径迹退火带上—下限温度为70~125℃。同石油主要形成于60~140℃之间相接近。此方法还可解决沉积盆地热历史及某些基础地质问题。裂变径迹年龄代表抬升剥蚀以后的地质年龄,可推断抬升剥蚀作用发生的时间。提出了用包裹体溫度认识地热过程。 准噶尔盆地地溫演化可分为三个主要阶段:地槽期(石炭纪时期)古地温梯度8~5℃/100m:山前坳陷期(二叠—三叠纪末)古地温梯度5~3℃/100m:地台期(侏罗—早第三纪)古地温梯度3~2℃/100m。盆地中几个主要凹陷内石炭、二叠系生油岩在二叠、三叠纪时就进入了生油高峰期,因之应特别重视寻找古生新储的油气藏。

     
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