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碳酸盐岩

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The contents of sand,shale or carbonate in complex formations can be obtained from logs of Elemental Capture Spectroscopy Sonde. The porosity and permeability calculated from the contents are comparatively better accordant to core data.

元素俘获谱测井利用定量测得的钙等多种元素的含量,计算岩石的碳酸盐岩含量,进而进行岩性识别和地层对比;利用ECS成果求出孔隙度、渗透率与岩心分析数据有较好的一致性;依据该岩石分类方法,做出单井的岩性剖面图,地层岩性的定性分析对比转化为岩性及其量化的对比划分。

As an important hydrocarbon reservoir, reefs and carbonates have great potential in oil exploration.

生物礁及碳酸盐岩储层是一种典型的油气储层,具有巨大的油气勘探潜力。

Stable isotopic compositions of carbon and oxygen in marine carbonates formed during geological history has long ...

地质历史时期碳酸盐岩氧、碳同位素组成的研究是目前国际上同位素地球化学研究中的一项重大课题。

Seismic imaging in Northeast Sichuan is greatly influenced by the widely distributional carbonate,strata juxtaposition with swelling and concaving,superimposition and connection between different wave fields,complex interlayer contact conditions,static corrections, high and steep structure ,as well as rapid change of seismic velocity in the area.

针对川东北地区碳酸盐岩高度发育,地层隆凹相间,各种波场交叉叠置,层间接触关系复杂,以及静校正问题、高陡构造及速度变化快等影响因素突出的特点,通过分析地表因素、有效波频率、静校正量及膏岩层效应对地震资料品质和成像的影响,研究和开发出三维折射波静校正以及构造建模层速度约束偏移成像等一系列处理技术,消除了众多因素对地震成像的影响,并在宣汉达县地区得到良好的应用效果,为普光特大气田的大规模开发奠定了基础。

Years of monitoring carbon cycle were carried out on 10 typical sites, and 47 points of deep source CO2 degassing in Tibet, Sichuan, and Yunan were investigated.

在对典型点定位监测的基础上,对碳酸盐岩岩溶作用的碳循环特点,特别是地质历史上碳汇变化的研究成果进行了初步总结。

ABSTRACT : The fractures are the main percolating c hannels of oil and gas in dense carbonate reservoirs.

摘 要 裂缝是致密碳酸盐岩储集层中油气的主要渗流通道。

The fractures are the main percolating channels of oil and gas in dense carbonate reservoirs.

裂缝是致密碳酸盐岩储集层中油气的主要渗流通道。

According to this scheme, the Longmaxi Formation is only referred to as the black siliceous and carbonaceous shales at the base of the Silurian strata. All the carbonate rocks above it have been redelineated and redivided into new lithostratigraphic units.

新方案除对志留系底的黑色硅质碳质页岩沿用龙马溪组这一岩石地层单位名称外,其上的碳酸盐岩均重新划分和建立了新的岩石地层单位,并确定其涵义和时限标准。

Lower Cretaceous belong to retrograding sedimentary sequence of tide-flat-carbonate platform facies,and have good hydrocarbon source rock and reservoir rock but no good cap rock.

下白垩统属退积的潮坪—碳酸盐岩台地沉积序列,生、储油层发育,但盖层发育相对较差,有可能在靠近改则—尼玛断裂带附近形成一些与逆冲断层有关的小型油气藏。

Molar-tooth structures refer to the aggregations of equal-axised or polygonal microspar calcite with a crystal size of 0.01mm and a clear boundary, which are mainly developed in the Precambrian fine-grained carbonate rocks. The morphology of Molar-tooth can be divided into ribboned, nodular and clastic forms.

臼齿构造是特指那些发育在前寒武纪细粒碳酸盐岩中有清晰边界、粒度在0.01mm左右的由等轴或多边形的微亮晶方解石组成的集合体,其形态可分为条带状构造、瘤状构造及棱角碎块状构造。

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