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Destruction of hydrocarbon reservoirs due to tectonic modifications: Conceptual models and quantitative evaluation on the Tarim Basin, China

机译:由于构造修改因碳氢化合物储层的破坏:中国塔里木盆地的概念模型与定量评价

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The Tarim Basin in China is a complicated superimposed basin with four periods of hydrocarbon accumulations and three periods of modifications due to tectonic movements, forming complicated hydrocarbon reservoirs, many of which have gone through reservoir migration, reservoir scale reformation, reservoir damage and phase alterations a result of the tectonic events. Due to the complexity, the hydrocarbon exploration in this region has low success drilling rate. It is of great importance to study the destruction to the early hydrocarbon accumulations by the tectonic movements and quantitatively evaluate the remaining resource for understanding the current hydrocarbon distribution and guiding the exploration. This study analyzed six periods of large tectonic events in the Tarim Basin, and found the destroyed hydrocarbon volume was mainly controlled by four geological factors, including the ratio of the destroyed to the original hydrocarbon amount, tectonic event number and sequence, and the cap seal capacity. Larger ratio of destroyed hydrocarbon, less tectonic event number, later sequence and stronger cap seal capacity lead to more hydrocarbons preserved through the tectonic events. Based on the geological analysis, we established quantitative relationships among the destroyed hydrocarbon volume by the tectonic events (Q(1)), the volume of primary hydrocarbon accumulation (Q(0)), the ratio of destroyed hydrocarbon (K-1), the tectonic event number (n) and sequence (i), and cap seal capacity (fc). Using these relationships and the calibrated geological parameters, we delineated the hydrocarbon accumulation and destruction history and quantified the hydrocarbon loss due to the tectonic events for both the Tazhong area and the whole Tarim Basin. In the Tazhong area, four major accumulation events occurred at 510 Ma, 298 Ma, 227 Ma and 38 Ma with each accumulation underwent 68%, 59%, 28% and 0% of hydrocarbon loss due to later tectonic events. In total, over 60% of the original hydrocarbon reserves have been destroyed in the Tarim Basin, with an estimate of ca. 1.9 billion tons remaining hydrocarbons in the Tazhong area. At present, more than 95% oil and gas reservoirs and over 93% high quality exploration wells are located in the areas with high remaining resource potential predicted in this study, whereas 70% non-commercial production wells are located outside. Overall, this work shows that a careful evaluation of the damage to reservoirs from tectonic events can considerably enhance the success rate of hydrocarbon exploration.
机译:中国的塔里木盆地是一种复杂的叠加盆,具有四个碳氢化合物积累,并且由于构造运动,形成复杂的烃藏,其中许多已经经历了水库迁移,储层规模改造,储层损伤和相变的变化构造事件的结果。由于复杂性,该地区的碳氢化合物勘探成功钻井率低。通过构造运动研究对早期碳氢化合物积聚的破坏并定量评估剩余资源,以了解当前的碳氢化合物分布和指导勘探。本研究分析了塔里木盆地的六个大型构造事件,发现破坏的烃体积主要由四个地质因素控制,包括被破坏与原始烃类,构造事件数和序列的比例,以及帽密封容量。被破坏的烃,更少的构造事件数,后来序列和更强的帽密封容量的较大比率导致通过构造事件保存的更多烃。基于地质分析,我们通过构造事件(Q(1)),初级烃体积(Q(0)),破坏烃(K-1)的比例建立了定量关系(Q(1)),构造事件数(n)和序列(i)和帽密封容量(fc)。使用这些关系和校准的地质参数,我们描绘了碳氢化合物积累和破坏历史,并由于塔宏地区和整个塔里木盆地的构造事件而量化了碳氢化合物损失。在塔宏地区,4个主要的积累事件发生在510 mA,298 mA,227 mA和38 mA,每次积累由于后来的构造事件导致的碳氢化合物损失的68%,59%,28%和0%。总共有超过60%的原始碳氢化合物储量在塔里木盆地被摧毁,估计是CA.塔洪地区剩余10亿吨碳氢化合物。目前,超过95%的石油和天然气储层和93%的高质量勘探井位于本研究中预测的高剩余资源潜力的地区,而70%的非商业生产井位于外面。总体而言,这项工作表明,仔细评估来自构造事件的储存器的损害可以大大提高碳氢化合物勘探的成功率。

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