| 山东蓬莱丹崖山角砾状石英岩特征及其成因 |
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| 引用本文： | 李殿河. 山东蓬莱丹崖山角砾状石英岩特征及其成因[J]. 山东国土资源, 1985, 0(2) |
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| 作者姓名： | 李殿河 |
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| 作者单位： | 山东省地质矿产局第三地质队 |
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| 摘 要： | 前言地学界专家与地学工作者来烟台地区参加学术会议或进行野外地质考察时,免不了要到蓬莱仙阁旅游一番。作为地学工作者,除了听神话般的介绍与饱览仙阁美景外,还会对其脚下的岩石发生极大的兴趣。当你踏上蓬莱阁大门“丹崖仙境”,经过院内的六块巨大的“坤爻石”直至后海崖“仙人洞”,如果留神观察会发现岩石全由角砾状石英岩碎块组成。该岩石为上元古界蓬莱群辅子夼组石英岩。
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CHARACTERISTICS OF THE BRECCIATED DANYASHAN QUARTZITE AND ITS ORIGIN IN THE PENGLAI REGION |
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| Li Dianhe. CHARACTERISTICS OF THE BRECCIATED DANYASHAN QUARTZITE AND ITS ORIGIN IN THE PENGLAI REGION[J]. SHANDONG LAND AND RESOURCES, 1985, 0(2) |
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| Authors: | Li Dianhe |
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| Abstract: | The brecciated Danyashan Quartzite which intercalates some of the brecciated slate in the Penglai region, Shandong Province belongs to the Fuzikuang formation of the Penglai series of the Proterozoic era. The origin and the characteristics of the breeciated quartzite are described. The author suggests that the brecciated quartzite belongs to the cryptoexplosion breccia which was related to the eruption of basalt during the Tertiary period and is neither sedimentary and syngenetic conglomerate, nor tectonic ... |
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