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An analysis of natural gas exploration potential in the Qiongdongnan Basin by use of the theory of “joint control of source rocks and geothermal heat”

机译:利用“烃源岩与地热联合控制”理论分析琼东南盆地天然气勘探潜力

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The Oligocene Yacheng Fm contains the most important source rocks that have been confirmed by exploratory wells in the Qiongdongnan Basin. The efficiency of these source rocks is the key to the breakthrough in natural gas exploration in the study area. This paper analyzes the hydrocarbon potential of each sag in this basin from the perspective of control of both source rocks and geothermal heat. Two types of source rocks occur in the Yacheng Fm, namely mudstone of transitional facies and mudstone of neritic facies. Both of them are dominated by a kerogen of type-III, followed by type-II. Their organic matter abundances are controlled by the amount of continental clastic input. The mudstone of transitional facies is commonly higher in organic matter abundance, while that of neritic facies is lower. The coal-measure source rocks of transitional facies were mainly formed in such environments as delta plains, coastal plains and barrier tidal flat-marshes. Due to the control of Cenozoic lithosphere extension and influence of neotectonism, the geothermal gradient, terrestrial heat flow value (HFV) and level of thermal evolution are generally high in deep water. The hot setting not only determines the predominance of gas generation in the deep-water sags, but can promote the shallow-buried source rocks in shallow water into oil window to generate oil. In addition to promoting the hydrocarbon generation of source rocks, the high geothermal and high heat flow value can also speed up the cracking of residual hydrocarbons, thus enhancing hydrocarbon generation efficiency and capacity. According to the theory of joint control of source quality and geothermal heat on hydrocarbon generation, we comprehensively evaluate and rank the exploration potentials of major sags in the Qiongdongnan Basin. These sags are divided into 3 types, of which type-I sags including Yanan, Lingshui, Baodao, Ledong and Huaguang are the highest in hydrocarbon exploration potential.
机译:渐新世崖城组含琼东南盆地勘探井已证实的最重要烃源岩。这些烃源岩的效率是该研究区天然气勘探取得突破的关键。本文从控制烃源岩和地热的角度分析了该盆地各凹陷的油气潜力。崖城组有两种类型的烃源岩,即过渡相泥岩和晚生相泥岩。两者均以III型干酪根为主,其后是II型干酪根。它们的有机质丰度受大陆碎屑输入量的控制。过渡相的泥岩中有机质丰度通常较高,而浅相​​的泥岩较低。过渡相煤系烃源岩主要形成在三角洲平原,沿海平原和潮汐屏障平坦沼泽等环境中。由于控制了新生代岩石圈扩展和新构造运动的影响,深水区的地热梯度,地面热流值(HFV)和热演化水平普遍较高。热定型不仅决定了深水凹陷中产气的优势,而且可以促进浅水中的浅埋烃源岩进入油窗以产生石油。除了促进烃源岩生烃外,高地热和高热流量值还可以加速残余烃的裂解,从而提高生烃效率和产能。根据源质量和地热联合控制油气生成的理论,我们对琼东南盆地主要凹陷的勘探潜力进行了综合评价和排序。这些凹陷分为3种类型,其中I型凹陷包括延安,陵水,宝岛,乐东和华光等油气勘探潜力最高。

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