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摘要:
The present study introduces the carbonatite in the northern part of the Korean Peninsula for the first time.Recent exploration and development of the phosphorus-bearing carbonate rocks in the area have accumulated new geological data which gave us an opportunity to study origin of the carbonate rocks.We conducted geological survey, geochemical analyses of trace elements and rare earth elements, and carbon and oxygen isotope analyses for the carbonatites from Ssangryong, Pungnyon, Yongyu and Puhung districts of the northern part of the Korean Peninsula.This research confirms that the phosphorus-bearing carbonate rocks are carbonatite originating from the mantle.The studied carbonatites are distributed at the junctions of ring and linear structures or around their margins and contain a greater amount of REEs, Y, and Sr than carbonate rocks.The carbonatites in Yongyu and Puhung area show evidence that they were formed from mantle plume generated at the lower mantle and display similar fractionation characteristics to carbonatites in Barrado Itapirapua in Brazil and Kalkfeld and Ondur-akorume in Namibia.REE patterns of the carbonatites are typical of carbonatites and the carbon and oxygen isotope analyses demonstrate that the carbonatites were originated from mantle.The carbonatites from the northern part of the Korean Peninsula have a great potential for sources of REE, Y, PGE(platinum group ele-ments), copper, and gold.
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篇名 Characteristics of carbonatites from the northern part of the Korean Peninsula:A perspective from distribution, geology and geochemistry
来源期刊 地学前缘(英文版) 学科
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年,卷(期) 2021,(1) 所属期刊栏目 Research Paper
研究方向 页码范围 173-181
页数 9页 分类号
字数 语种 英文
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地学前缘(英文版)
双月刊
1674-9871
11-5920/P
16开
北京市海淀区学院路29号中国地质大学(北京)《地学前缘》英文刊编辑部
2010
eng
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1146
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