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首页> 外文期刊>Journal of Applied Sciences >The Types of Clay Minerals in the Kongdian Formation (Upper Part), South Slope of the Dongying Depression, East China
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The Types of Clay Minerals in the Kongdian Formation (Upper Part), South Slope of the Dongying Depression, East China

机译:东营凹陷南坡孔店组(上部)黏土矿物类型

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The Upper part of the Kongdian formation of the Paleocene-Eocene age consists mainly of fine to medium feldspathic sandstone. Samples analyzed are from depths of 1572.55 to 2298m, representing a temperature range of 60.5 to 88.5 °C. The authigenic cla
机译:古新世-始新世的孔店组的上部主要由精细到中等的长石质砂岩组成。分析的样本来自1572.55至2298m的深度,代表60.5至88.5°C的温度范围。自生类

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