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内蒙古大石寨地区稀土元素的区域分布特征
引用本文:杨帆,宋云涛,张舜尧,郝志红,郭志娟,王成文,岑况.内蒙古大石寨地区稀土元素的区域分布特征[J].现代地质,2016,30(4):802-810.
作者姓名:杨帆  宋云涛  张舜尧  郝志红  郭志娟  王成文  岑况
作者单位:1中国地质科学院 地球物理地球化学勘查研究所,河北 廊坊065000; 2中国地质大学(北京)地球科学与资源学院,北京100083
基金项目:中国地质调查局地质大调查项目(1212011220598,1212010050304,121201108000150002-03);中央级公益性科研院所基本科研业务费专项(YYWF201514,AS2014J02);国土资源部公益性行业科研专项(201411024)
摘    要:总结了内蒙古大石寨地区1∶25万区域地球化学调查获得的1点/4km2的水系沉积物组合样品中的La、Ce、Pr、Nd、Sm、Eu、Gd、Tb、Dy、Ho、Er、Tm、Yb、Lu、Y等15种稀土元素的区域地球化学分布特征。稀土元素分布与研究区中部的黑云母花岗岩密切相关,轻稀土主要分布在该岩体外围的二叠系地层中,重稀土主要分布在该岩体上方。该岩体上方和外围地层的稀土元素分布、稀土元素总量、轻重稀土比及δCe、δEu、(La/Sm)N、(La/Tb)N、(La/Lu)N、(Ce/Yb)N、(Gd/Lu)N等稀土元素分馏特征的差异明显。利用区域地球化学调查水系沉积物样品中的稀土元素含量,可获得研究区可靠的稀土元素区域地球化学分布特征,也可反映研究区地质特点,并为区域地球化学异常解译提供参考资料。

关 键 词:区域地球化学调查  水系沉积物  稀土元素  大石寨地区  异常解译  

Regional Geochemical Distribution Characteristics of Rare Earth Elements in the Dashizhai Area,Inner Mongolia
YANG Fan,SONG Yuntao,ZHANG Shunyao,HAO Zhihong,GUO Zhijuan.Regional Geochemical Distribution Characteristics of Rare Earth Elements in the Dashizhai Area,Inner Mongolia[J].Geoscience——Journal of Graduate School,China University of Geosciences,2016,30(4):802-810.
Authors:YANG Fan  SONG Yuntao  ZHANG Shunyao  HAO Zhihong  GUO Zhijuan
Institution:1Institute of Geophysical and Geochemical Exploration, CAGS, Langfang,Hebei065000, China; 2School of Earth Sciences and Resources, China University of Geosciences, Beijing100083, China
Abstract:Based on the regional geochemical survey, stream sediment sampling and analysis, the REE distribution characteristics of the stream sediments from the Dashizhai area in Inner Mongolia were evaluated systematically. Results show that ΣREE, ΣLREE/ΣHREE, δCe, δEu, (La/Sm)N, (La/Tb)N, (La/Lu)N, (Ce/Yb)N and (Gd/Lu)N of stream sediments have significant differences from the biotite granite in the central part of the study area and strata around the biotite granite. The REE distribution is closely related to the biotite granite; light rare earth elements are mainly distributed in the periphery of the biotite granite, and heavy rare earth elements are mainly distributed in the top of that biotite granite. The REE concentration of stream sediments from regional geochemical survey can reasonably describe the REE distribution, and can reflect the geological characteristics of the survey area, thus can provide references for the interpretation of regional geochemical anomalies.
Keywords:regional geochemical survey  stream sediment  rare earth element  Dashizhai area  interpretation of anomaly  
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