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首页> 外文期刊>Carbonates And Evaporites >Identification of Neogene mixed lacustrine carbonate in western Qaidam basin
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Identification of Neogene mixed lacustrine carbonate in western Qaidam basin

机译:柴达木盆地西部新近纪混合湖相碳酸盐岩的识别

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Compared with marine carbonate, lacustrine carbonate is limited in distribution globally; moreover, as an unconventional kind of carbonate, it cannot be evaluated and identified with conventional methods, so less attention has been paid and fewer studies have been made on it. However, according to exploration experiences all over the world, lacustrine carbonate can be an important source rock and reservoir rock in some cases. Qaidam basin, a large salt-water lake basin, had the lacustrine mixed deposition setting to form complex carbonate reservoirs. The recently found Neogene lacustrine algal limestone is an exploration target worthy of attention. The author has used drilling and well logging data to identify lacustrine algal limestone. The method is of great significance for the exploration and development of lacustrine carbonate in other areas.
机译:与海洋碳酸盐相比,湖相碳酸盐在全球范围内分布有限;此外,作为一种非常规的碳酸盐,无法用常规方法进行评估和鉴定,因此受到的关注较少,对其的研究也较少。但是,根据世界各地的勘探经验,在某些情况下,碳酸盐湖相可能是重要的烃源岩和储集岩。柴达木盆地是一个大型的咸水湖盆地,其湖床混合沉积环境形成了复杂的碳酸盐岩储集层。最近发现的新近纪湖相藻灰岩是一个值得关注的勘探目标。作者使用钻井和测井数据来识别湖相藻类石灰石。该方法对其他地区的湖相碳酸盐岩的勘探开发具有重要意义。

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