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首页> 外文期刊>Marine and Petroleum Geology >Petroleum generation characteristics of heterogeneous source rock from Chia Gara formation in the Kurdistan region, northern Iraq as inferred by bulk and quantitative pyrolysis techniques
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Petroleum generation characteristics of heterogeneous source rock from Chia Gara formation in the Kurdistan region, northern Iraq as inferred by bulk and quantitative pyrolysis techniques

机译:散装和定量热解技术推断伊拉克北部库尔德斯坦地区奇亚加拉地层非均质烃源岩的石油生成特征

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This study is the first attempt which provides information regarding the bulk and quantitative pyrolysis results of the Chia Gara Formation from the Kurdistan region, northern Iraq. Ten representative early mature to mature samples from the Chia Gara Formation were investigated for TOC contents, Rock Eval pyrolysis, pyrolysis-GC and bulk kinetic parameters. These analyses were used to characterize the petroleum generated during thermal maturation of the Chia Gara source rock and to Aarify the quantity of the organic matter and its effect on the timing of petroleum generation. Pyrolysis HI data identified two organic facies with different petroleum generation characteristics; Type II-III kerogen with HI values of >250 mg HC/g TOC, and Type III kerogen with HI values < 100 mg HC/g TOC. These types of kerogen can generate liquid HCs and gas. This is supported by the products of pyrolysis gas chromatography (Py-GC) analysis of the extracted rock samples. Pyrolysis products show a dominance of a marine organic matter with variable contributions from terrestrial organic matter (Types II III and III kerogen), and produces mainly paraffinic-naphthenic-aromatic low wax oils with condensate and gas. Bulk kinetic analysis of the Chia Gara source rock indicates a heterogeneous organic matter assemblage, typical of restricted marine environments in general. The activation energy distributions reveal relatively broad and high values, ranging from 40 to 64 kcal/mol with pre-exponential factors varying from 2.2835 E+12/sec to 4.0920 E+13/sec. The predicted petroleum formation temperature of onset (TR 10%) temperatures ranges from 110 to 135 degrees C, and peak generation temperatures (geological T-max) between 137 degrees C and 152 degrees C. The peak generation temperatures reach a transformation ratio in the range of 42-50% TR, thus the Chia Gara source rock could have generated and expelled significant quantities of petroleum hydrocarbons in the Kurdistan of Iraq. (C) 2016 Elsevier Ltd. All rights reserved.
机译:这项研究是首次尝试,提供有关伊拉克北部库尔德斯坦地区Chia Gara地层的大量和定量热解结果的信息。研究了来自Chia Gara组的10个代表性的早熟至成熟样品的TOC含量,岩石评估热解,热解GC和整体动力学参数。这些分析用于表征Chia Gara烃源岩热成熟过程中产生的石油,并分析有机物的数量及其对石油生成时间的影响。热解HI数据确定了两个具有不同石油生成特征的有机相。 HI值> 250 mg HC / g TOC的II-III型干酪根,HI值<100 mg HC / g TOC的III型干酪根。这些类型的干酪根可产生液态HC和气体。这由提取的岩石样品的热解气相色谱(Py-GC)分析产品支持。热解产物显示出海洋有机物占主导地位,而陆地有机物(II III型和III型干酪根)的贡献则不同,并且主要生产具有凝析油和天然气的链烷烃-环烷烃-芳族低蜡油。对Chia Gara烃源岩进行的块体动力学分析表明,有机质组分是非均质的,通常在受限的海洋环境中很典型。活化能分布显示出相对较宽和较高的值,范围从40到64 kcal / mol,预指数因子从2.2835 E + 12 / sec到4.0920 E + 13 / sec。预测的开始(TR 10%)温度的石油形成温度范围为110至135摄氏度,峰值生成温度(地质T-max)介于137摄氏度和152摄氏度之间。 TR范围为42-50%,因此Chia Gara烃源岩可能在伊拉克库尔德斯坦产生并排出了大量石油烃。 (C)2016 Elsevier Ltd.保留所有权利。

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