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ГЕОТЕРМИЯ И ОЦЕНКА НЕФТЕГАЗОВОГО ПОТЕНЦИАЛА БУРЕИНСКОГО БАССЕЙНА (ДАЛЬНИЙ ВОСТОК РОССИИ)

机译:地热和评价Buzein盆地(俄罗斯远东)的石油和天然气潜力

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摘要

The relevance. The Bureya sedimentary basin is the most interesting in respect of oil and gas intermountain basin of frontier mainland of Russian Far East. An upbeat assessment of prospects of oil and gas field discovery in the basin is proved by the results of previous prospecting work and scientific research. The aim of this paper is further argumentation of hydrocarbon prospects of upper Jurassic-lower Cretaceous deposits in the Bureya basin based on the use of domestic basin modeling software TeploDialog, having original features. Study object is middle-upper Jurassic, upper Jurassic-lower Cretaceous and Cretaceous sedimentary sequences of the Kyndal graben, the most studied structure in the Bureya fore deep. The previous investigations have revealed that the whole Jurassic-Cretaceous section of the Bureya basin is involved in oil-and-gas formation. Methods. In the software TeploDialog the paleotemperature modeling method is implemented based on the numerical solution of heat transfer equation of a horizontally layered solid with a movable upper boundary. Mathematical model includes climatological secular trend of temperatures on the earth surface (boundary condition) and paleotemperatures from vitrinite reflectance evaluation (observational). The method does not require a priori information about the nature and magnitude of the deep heat flow, the heat flow is determined by the solution of the geothermal inversion within the framework of parametric description of the sedimentation history and the history of the thermophysical properties of sedimentary strata. Results. The study found that geothermy of graben since Jura permitted formation of liquid hydrocarbons in the sedimentary cover rocks, which could begin about 107 million years ago, in the middle of the Alb. The most intensive oil generation took place in the period of 107–40 million years ago, until the middle of the Eocene. Temperature conditions for the generation of liquid hydrocarbons are still the same for talyndzhansky kitchen. Maximal duration of temperature periods, favourable for gas formation is observed in chemcukinsky kitchen. The conditions for gas generation are still the same for urgalsky and chegdomynsky kitchens. The results obtained using the domestic software TeploDialog and previously obtained in software PetroMod, strongly aligned. These computer programs are characterized by different approaches to consideration of tectonic-sedimentation and thermal conditions of hydrocarbon generation. Therefore, the results of this study are an additional argument for the positive prospects of oil and gas potential of the upper Jurassic-lower Cretaceous deposits of the Bureya basin.
机译:相关性。 Bureya沉积物盆地是俄罗斯远东地区边境内地石油和天然气盆地最有趣的。通过先前勘探工作和科学研究的结果证明了盆地中石油和天然气场发现前景的乐观评估。本文的目的是基于使用国内盆地建模软件Teplodialog,具有原始特征的Bureya盆地中侏罗腊纳盆地上层白垩纪沉积物的碳氢化合物前景的讨论。研究对象是克yndalGraben的中上部侏罗纪,上侏罗腊纳较低的白垩纪和白垩纪沉积序列,深层树木酵母中最多研究的结构。之前的调查显示,Bureya盆地的整个侏罗纪 - 白垩纪部分参与油气形成。方法。在软件中,TEPLODIALOG基于具有可移动上边界的水平分层固体的传热方程的数值解,实现了古间度建模方法。数学模型包括地球表面(边界条件)温度的气候性气温和来自vitriinite反射率评估(观察)的古鳃物。该方法不需要关于深热流动性质和大小的先验信息,通过参数化历史的参数描述框架内的地热反转和沉积热物理特性的历史来确定热流来确定热流。地层。结果。该研究发现,自汝拉在沉积盖岩石中允许形成液体烃的地质以来,可以在AGB的中间开始,在大约1.7亿年前开始。最密集的石油一代人在107-40万年前发生,直到蚕食中部。液体碳氢化合物的温度条件对于Talyndzhansky厨房仍然是一样的。在Chemcukinsky厨房中观察到最大持续时间,有利于气体形成。乌尔卡尔基和Chegddomynsky厨房的气体产生条件仍然是一样的。使用国内软件Teplodialog获得的结果,并在软件PetroMod中获得,强烈对齐。这些计算机程序的特征在于考虑构造沉降和烃生成的热条件的不同方法。因此,该研究的结果是对Bureya盆地的上侏罗腊纳 - 下白垩纪沉积物的水和气体潜力的积极前景的额外争论。
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