| 东营凹陷岩盐成矿条件浅析 |
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| 引用本文： | 孙文广,刘丰武,彭文泉,蒋波,高庆,王峰,赵海滨.东营凹陷岩盐成矿条件浅析[J].山东地质,2009(3):27-30. |
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| 作者姓名： | 孙文广 刘丰武 彭文泉 蒋波 高庆 王峰 赵海滨 |
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| 作者单位： | 山东省第一地质矿产勘查院,山东济南250014 |
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| 摘 要： | 东营凹陷是一个中、新生代断落凹陷区，发育了巨厚的新生代地层。凹陷内岩盐主要发育在沙河街组四段中下部，通过对沉积盆地演化阶段、岩盐赋存层位及蒸发岩系序列结构的分析，指出岩盐是在陆相环境中沉积的，属海源陆相沉积矿床。
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| 关 键 词： | 岩盐 蒸发岩系 成盐模式 东营凹陷 |
Primary Study on Salt mforming Condition in Dongying Depression |
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| Institution: | SUN Wen--guang, LIU Feng--wu, PENG Wen--quan, JIANG Bo, GAO Qing, WANG Feng, ZHAO Hai-- bin (No. 1 Exploration Institute of Geology and Mineral Resources, Shandong Jinan 250014, China) |
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| Abstract: | Dongying depression is a Mesozoic and Cenozoic sag drop area. It developed thick Cenozoic strata. Dongying depression halite mainly developed in middle and lower part of the fourth section of Shahejie formation. The ore--bearing strata are sedimented in continental sedimentary environment. It belongs to marine facies continental sedimentary deposits. |
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| Keywords: | Rock salt evaporation rock system salt--forming mode Dongying depression |
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