| 海南岛东部黄竹岭地区“抱板群”的解体 |
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| 引用本文： | 龙文国,符策锐,朱耀河.海南岛东部黄竹岭地区“抱板群”的解体[J].地层学杂志,2002,26(3):212-215. |
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| 作者姓名： | 龙文国 符策锐 朱耀河 |
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| 作者单位： | 海南地质矿产局,海南海口,570206 |
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| 基金项目： | 国家地质调查局区域调查项目，， |
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| 摘 要： | 1/ 5万填图结果表明 ,黄竹岭地区的原“抱板群”实际上包含了时代不同、环境不同的二套物质建造 ,抱板群应予以解体 ,其中黄竹岭南侧的中、浅中变质沉积—火山岩系与海南岛其他地区的南碧沟组可对比 ,地质时代为奥陶纪 ;剔除此之后的一套中深变质沉积—火山岩系为海南岛真正意义的抱板群
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| 关 键 词： | 抱板群 南碧沟组 黄竹岭 奥陶系 元古代 海南岛 |
| 文章编号： | 0253-4959(2002)03-0212-04 |
| 修稿时间： | 2002年4月1日 |
DISINTEGRATION OF THE BAOBAN GROUP IN HUANGZHULING AREA OF EASTERN HAINAN ISLAND |
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| LONG Wen guo,Fu Ce rui,and ZHU Yao he.DISINTEGRATION OF THE BAOBAN GROUP IN HUANGZHULING AREA OF EASTERN HAINAN ISLAND[J].Journal of Stratigraphy,2002,26(3):212-215. |
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| Authors: | LONG Wen guo Fu Ce rui and ZHU Yao he |
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| Abstract: | mapping indicates that the original “Baoban Group” should be disintegrated into two parts which are of different ages and were formed in different tectonic settings. The first is volcanic sedimentary series in south of Huangzhouling mountain. The second is newly difined Baoban Group in east and west of Huangzhouling mountain, which was deposited during the middle late Proterozoic. |
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| Keywords: | Baoban Group Nanbigou Formation Huangzhouling Hainan island Ordovician Proterozoic |
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