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首页> 外文期刊>Open Journal of Geology >Source Rock Evaluation and 1-D Basin Modelling Approach for the Sargelu Formation, Atrush-2 Well, Kurdistan Region-Iraq
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Source Rock Evaluation and 1-D Basin Modelling Approach for the Sargelu Formation, Atrush-2 Well, Kurdistan Region-Iraq

机译:Sargelu Clowation,Atrush-2井,Kurdistan Region-Iraq的源岩体评估和1-D盆地建模方法

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The present study focuses on source rock evaluation of the Sargelu Formation by using core chips of rocks collected from well Atrush-2, Duhok, Kurdistan Region-Iraq. The Rock-Eval pyrolysis and vitrinite reflectance were executed. Subsequently, the selected parameters were used for source rock evaluation and 1-D Basin Modelling calibration. The upper part of the formation mainly comprises argillaceous limestone with low content of organic matter (0.64% - 1% TOC). By contrast, the lower part is dominated with shale interval and contains high amounts of TOC values (>4% for 1272 - 1278 m) reveling good to very good quality source rock. Accordingly, good to very good hydrocarbon generation potential is suggested for this formation. Organic matter of the Sargelu Formation contains type II and mixed-type II-III kerogen. The values of Tmax and vitrinite reflectance (Ro%) demonstrate that the formation is thermally mature and in the oil zone. In order to construct a thermal history of the formation and determine the timing of hydrocarbon maturation and generation, the 1-D basin modelling PetroMod 2019.1 was used in this study. Based on the 1-D Basin modelling simulation and its outputs, about 3500 m of overburden have been eroded at the study area. The present-day heat flow was found to be 30 mW/m2. The organic matter of Sargelu Formation entered the early oil zone in 64 Ma and reached the main oil zone ca. 5 Ma. The formation is still in the main oil zone at present-day. In well Atrush-2, the highest rate of oil generation for the Sargelu Formation was in the 8.5 Ma, the onset of oil expulsion from Sargelu Formation was in 50 Ma and the expulsion mass has been reached 0.5 Mtons at present-day.
机译:本研究侧重于使用从Hont Helush-2,Kurdistan Region-Iraq井中收集的岩石的岩石芯片对Sargelu形成的源岩评价。执行岩石 - 醇热解和vitriinite反射率。随后,所选参数用于源岩评估和1-D盆地建模校准。该形成的上部主要包括具有低含量的有机物质(0.64% - 1%TO C)的骨质石灰石。相比之下,下部用页岩间隔主导,含有大量的TOC值(> 4%,1272 - 1278米)令人陶醉于非常好的质量源岩石。因此,提出了对这种形成的良好的碳氢化合物产生潜力。 Sargelu形成的有机物含有II型和混合型II-III Kerogen。 Tmax和vitriinite反射率(RO%)的值表明,形成是热成熟的和油区。为了构建地层的热历史并确定烃成熟和产生的时间,在本研究中使用了1-D盆地模型PetroMod 2019.1。基于1-D盆地建模仿真及其产出,在研究区已经侵蚀了大约3500米的覆盖物。发现本日热流为30mW / m 2。 Sargelu形成的有机物进入了64 mA的早期油区,并达到了大型油区。 5马。在当今,该形成仍在主油区。在宿舍-2井中,Sargelu形成的最高速率是8.5 mA,从萨格鲁形成的油排出的发作是在50 mA中,目前的排出量已达到0.5 mtons。

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