| 沂沭断裂带南段莱阳群的发现及其地质特征 |
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| 引用本文： | 肖丙建.沂沭断裂带南段莱阳群的发现及其地质特征[J].山东国土资源,2001,17(5):18-23. |
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| 作者姓名： | 肖丙建 |
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| 作者单位： | 山东省第七地质矿产勘查院,山东,临沂,276006 |
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| 摘 要： | 临沂至郯城一带青山群八亩地组火山岩之下存在大面积中生代陆相沉积.过去一直都划为王氏群.本文据其产出层位、岩石组合、古生物特征和区域对比关系,将其划分为莱阳群.
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| 关 键 词： | 莱阳群 地质特征 沂沭断裂带 |
| 文章编号： | 1009-0258(2001)05-0018-06 |
| 修稿时间： | 1998年8月1日 |
Found of Laiyang Group and Its Geological Characteristics in South Part of Yishu Faults |
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| XIAO Bing-jian.Found of Laiyang Group and Its Geological Characteristics in South Part of Yishu Faults[J].Land and Resources in SHANDONG Province,2001,17(5):18-23. |
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| Authors: | XIAO Bing-jian |
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| Abstract: | Mesozoic continental deposits widely occur under Bamudi formation (subvolcanic rocks) of Qingshan group from Linyi to Tancheng. It has been named Wangshi group up to now. According to its occurrence position, rock combinations, palaeo-biocharacteristics and regional contrast, it should be named Laiyang group. |
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| Keywords: | Laiyang group geological characteristics Yishu fault |
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