首页> 外文期刊>Arabian journal of geosciences >Sedimentary characteristics of braided stream-braided fan of Shawan Formation in Chunfeng Oilfield, northwest margin of Junggar Basin, China
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Sedimentary characteristics of braided stream-braided fan of Shawan Formation in Chunfeng Oilfield, northwest margin of Junggar Basin, China

机译:准gar尔盆地西北缘春风油田沙湾组辫状辫状扇沉积特征

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On the foundation of the geological background, textural maturity analysis, compositional maturity analysis, mudstone color index study, and other provenance research approach were fully made use of during this study to make certain the provenance of Shawan Formation in Chunfeng Oilfield. Provenance analysis of the Shawan Formation in Chunfeng Oilfield, conducted as the first stage of this study, revealed that the main provenance direction changed from northeast to northwest gradually, with a little fluctuation, while Shawan Formation was deposited. And then synthetically using seismic data, log data, and drilling data, according to petroleum geology and reservoir sedimentology, this study analyzed the sedimentary facies indicators, single-well facies, and logging facies in Shawan Formation; clarified the distribution of the sandbodies; and reached new insights on the types of the sedimentary facies of Shawan Formation in Chunfeng Oilfield. The research indicated that braided streams were developed during the deposition of the first member of Shawan formation and in the following two periods where braided fans became dominant little by little. These three microfacies, braided channel, channel bar, and braided plain, make up a typical stacked upward-fining cycle in the braided stream system. And the braided streams flowed from the northwest to the southeast in the research region, while the first member of Shawan Formation was formed. While the second member of Shawan Formation was deposited, the braided streams shrank gradually, and the braided fan coming from the northwest began to grow, with the flow direction moving from the northwest to the northeast. From the upstream to the downstream, the braided fan can be divided into three subfacies, proximal fan, middle fan, and distal fan. And when the third member of Shawan Formation was developed, the area of the braided fan became even larger than ever before, covering over almost the whole Chunfeng Oilfield.
机译:在地质背景的基础上,充分利用构造成熟度分析,成分成熟度分析,泥岩颜色指数研究等种源研究方法,确定了春风油田沙湾组物源。作为研究的第一阶段,对春峰油田沙湾组进行物源分析,结果表明,主要物源方向从东北向西北逐渐变化,波动很小,而沙湾组沉积。然后根据地震地质,测井数据和钻井数据,根据石油地质和储层沉积学,综合分析了沙湾组的沉积相指标,单井相和测井相。弄清沙体的分布;对春风油田沙湾组沉积相类型有新的认识。研究表明,辫状流是在沙湾组第一段沉积期间以及随后的两个时期逐渐形成的,在此期间辫状扇逐渐占主导地位。这三个微相,即辫状河道,河道横条和辫状平原,构成了辫状流系统中典型的堆叠向上细化循环。辫状流从研究区的西北向东南流动,形成了沙湾组的第一段。在沙湾组第二段沉积过程中,辫状流逐渐萎缩,来自西北的辫状扇开始生长,其流动方向从西北向东北移动。从上游到下游,编织风扇可分为三个亚相,即近端风扇,中间风扇和远端风扇。沙湾组第三段开发完成后,辫状扇的面积比以往任何时候都更大,几乎覆盖了整个春风油田。

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