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恢复模型
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  recovery model
    By comprehensive consideration over the effect of diagenetic compaction and organic matter thermalevolution and types ,a new organic carbon recovery model is established in this paper on the principle thatthe absolute content of unavailable carbon in kerogen remains constant in the pr0cess 0f hydrocarbon generation.
    本文综合考虑了成岩压实、有机质热浪化和类型的影响,以干酪根中无效欣在生烃过程中其绝对含量保持恒星这一原则,建立起一个新的有机碳恢复模型
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  recovery model
Annual survival probability was estimated at 0.85 (95% CI 0.75-0.92) using a recovery model and at 0.85 (95% CI 0.83-0.87) using an open robust design model.
      
Optimal control of production and remanufacturing in a simple recovery model with linear cost functions
      
A thixotropic recovery model has been developed that is based on consideration of the microstructural interactions that occur between particles within a suspension particle network.
      
The b-wave recovery model allows differentiation between two independent mechanisms contributing to the b-wave recovery process.
      
Failure detection and consensus in the crash-recovery model
      
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Based on digesting and absorbing advanced models at home and abroad, the system boundary and main events of petroleum geologic processes were determined with theories of information system and the simulation system of hydrocarbon migration and accumulation in sedimentary basins was developed. This modeling system includes four parts, parameter input, main assemblies of modules, mid-data chain, result output. The dominant part of modules consists of restoring original thickness module, sediment compaction module,...

Based on digesting and absorbing advanced models at home and abroad, the system boundary and main events of petroleum geologic processes were determined with theories of information system and the simulation system of hydrocarbon migration and accumulation in sedimentary basins was developed. This modeling system includes four parts, parameter input, main assemblies of modules, mid-data chain, result output. The dominant part of modules consists of restoring original thickness module, sediment compaction module, abnormally pressure evolution module, hydrocarbon generation module, and migration and accumulation module. T his system was applied to two typical basins of Jiuxi basin in Western China, and Bohai Bay basin in Eastern China. It has been demonstrated by practical data with high precision of simulation. Results show that models of system is effective. The system can be applied to any stage of an exploration basin or area, and can meet the requirement of input data for amount and mass.

在吸收消化国外先进模型基础上,以信息系统论思想确定了以油气运移聚集为核心的石油地质过程系统边界及主要事件;研制开发了沉积盆地油气运移聚集计算机模拟系统。该系统主要由4大部分构成:参数输入部分、模型主部件、中间数据链、成果输出部分,模型主部件包括原始厚度恢复模型、沉积压实、异常地层压力演化模型、成烃模型、油气运移聚集模型。系统在中国东部的渤海湾盆地、西部酒西盆地得到广泛应用检验,取得了满意的效果。

epositonal process can be reproduced dynamically on the basis of the restored fossil strata thickness by means of computer. The restored model of compacted thickness and the conversion formula of △t to of this area was estabilished for the first time. The erosive thickness of the strata in the end of Eogene was restored. The fossil thickness' of continuous anddiscontiouous strata was restored by reversal method. The depositional growth history of different depressions was analysed and compared dynamically on...

epositonal process can be reproduced dynamically on the basis of the restored fossil strata thickness by means of computer. The restored model of compacted thickness and the conversion formula of △t to of this area was estabilished for the first time. The erosive thickness of the strata in the end of Eogene was restored. The fossil thickness' of continuous anddiscontiouous strata was restored by reversal method. The depositional growth history of different depressions was analysed and compared dynamically on the basis of the drawn burial history diagram for single well and the diagram of deposition range comparison. The stratigraphic horizon with oil and gas and the time of generating and discharging hydrogen for the potential source rock is predicted. In the end,the best favorable area is pointed out.

地层埋藏史研究是借助计算机恢复地层古厚度,动态地再现盆地的沉积发育过程.本文在泥岩压实研究的基础上,首次建立了该区的压实厚度恢复模型和泥质岩声波时差与孔隙度的转换关系,恢复了旱第三纪末期地层的剥蚀厚度.利用反演法恢复了连续沉积地层和不连续沉积地层的古厚度.编绘了单井埋藏史图和沉降幅度对比图等.在此基础上动态地对比分析了研究区不同凹陷的沉积发育史,并预测了可能的生油气层段和可能油源岩的生烃、排烃时期和条件.指出了有利的油气远景区.

By comprehensive consideration over the effect of diagenetic compaction and organic matter thermalevolution and types ,a new organic carbon recovery model is established in this paper on the principle thatthe absolute content of unavailable carbon in kerogen remains constant in the pr0cess 0f hydrocarbon generation. On this basis, a calculation formula about hydrocarbon generation and discharge amount fit for geochemical logging is obtained to make the whole calculation process more correct and efficient than...

By comprehensive consideration over the effect of diagenetic compaction and organic matter thermalevolution and types ,a new organic carbon recovery model is established in this paper on the principle thatthe absolute content of unavailable carbon in kerogen remains constant in the pr0cess 0f hydrocarbon generation. On this basis, a calculation formula about hydrocarbon generation and discharge amount fit for geochemical logging is obtained to make the whole calculation process more correct and efficient than for mer illustration method. This new method has been applied successfully in geochemical logging to the offshore, subaerial and peripheral basins of the Liaohe Oil Field. In this paper, only one well in the TielingBasin is taken for example to explain the application of this method .The geochemical log of Dichang 2 well in the Tieling Basin shows that its hydrocarbon generation intensity is 263. 794 × 104t/km2,its hydrocarbon discharge intensity is 138. 166×104t/km2 and its resource density is 13. 190 ×104t/km2. All these have come up to the hydrocarbon-generating intensity standard for Ⅰ-typed oil and gas basins of our country.The Changtu Depression has more sufficient source of oil and gas, and is hoped to form some middle and small scale of oil and gas fields. The next exploration program is mainly to find traps and favorable reservoirs.

本文综合考虑了成岩压实、有机质热浪化和类型的影响,以干酪根中无效欣在生烃过程中其绝对含量保持恒星这一原则,建立起一个新的有机碳恢复模型。在此基础上得出了适用于地化录并应用的生、排烃量计算公式,从而使整个过程比以前的图解法更加准确、高效。本方法已成功地应用于辽河油田海上、陆上和外盆地的地优录并。但本文中仅以铁岭盆地的一口井为例说明了该方法的应用。铁岭盆地昌参2井的地化录井表明,其生径强度为263.794×104t/kin2,排烃强度为138.166×104t/km2,资源密度为13.190×104t/km2,达到了我国Ⅰ类含油气盆地的生烃强度标准,昌图凹陷具有较为充足的油气来源,可望形成一些中、小型油气田,下一步勘探的方向主要是寻找圈闭和有利的储层。

 
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