Geochemical Characteristics of Rare Earth Elements in Deep Geological Profile of Qitianling Intrusion, Hunan Province
Baishidu-Feixianzhen profile in Qitianling intrusion of Hunan Province is one of the most important profiles carried out in Sinoprobe. Despite the fact that a large amount of previous research had been carried out using various methods on rare earth elements (REEs) characteristics of Qitianling gran...
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Science Press, PR China
2014-01-01
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Online Access: | http://www.ykcs.ac.cn/cn/article/id/f761ec14-7dd7-454d-b16e-f885a3d03fa4 |
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author | HE Han-han LI Jian-kang LI Chao SU Xiao-yun ZHAO Zhi ZHANG Yi-jun WANG Guo-rui |
author_facet | HE Han-han LI Jian-kang LI Chao SU Xiao-yun ZHAO Zhi ZHANG Yi-jun WANG Guo-rui |
author_sort | HE Han-han |
collection | DOAJ |
description | Baishidu-Feixianzhen profile in Qitianling intrusion of Hunan Province is one of the most important profiles carried out in Sinoprobe. Despite the fact that a large amount of previous research had been carried out using various methods on rare earth elements (REEs) characteristics of Qitianling granite complex, no systematical study has been undertaken on geochemical characteristics from different geological units including limestone, sandstone, quaternary eluvial clays, the plution and the weathering crust. Analysis of the REEs in the profile through Inductively Coupled Plasma-Mass Spectrometry (ICP-MS) has been carried out and is reported in this paper. The results indicate that all geology units have LREE enrichment pattern, while a great difference exists between ΣREEs. For the total content of REEs in Qitianling Granite, the weathering crust has the highest level of ΣREEs with an average value of 605×10-6, and the limestone has the least ΣREEs with an average value of 154.3×10-6. In addition, the closer to the intrusions, the higher ΣREEs contents have in strata, even for the same lithology rock. In combination with REE-Y/ΣREE, ΣREE-δEu diagrams and Os Isotope tracer results, Qitianling granitoids might have mixed with some mantle materials. The content of REEs in the Qitianling Granite weathering crust (average value of RE2O3 is 814.8×10-6) are more than the cutoff grade of ion-absorbed-type REEs deposit (HREE RE2O3 0.05% and LREE 0.07%) in the main, which deserves further exploration. |
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spelling | doaj.art-d953777760154eee9309b9372c17c0432023-02-09T07:15:36ZengScience Press, PR ChinaYankuang ceshi0254-53572014-01-01331110117ykcs-33-1-110Geochemical Characteristics of Rare Earth Elements in Deep Geological Profile of Qitianling Intrusion, Hunan ProvinceHE Han-han0LI Jian-kang1LI Chao2SU Xiao-yun3ZHAO Zhi4ZHANG Yi-jun5WANG Guo-rui6Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China;Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China;National Research Center for Geoanalysis, Beijing 100037, China;School of Earth Sciences and Resources, China University of Geosciences (Beijing), Beijing 100083, China;Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China;Southern Hunan Institute of Geology and Survey, Chenzhou 423000, ChinaInstitute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China;Baishidu-Feixianzhen profile in Qitianling intrusion of Hunan Province is one of the most important profiles carried out in Sinoprobe. Despite the fact that a large amount of previous research had been carried out using various methods on rare earth elements (REEs) characteristics of Qitianling granite complex, no systematical study has been undertaken on geochemical characteristics from different geological units including limestone, sandstone, quaternary eluvial clays, the plution and the weathering crust. Analysis of the REEs in the profile through Inductively Coupled Plasma-Mass Spectrometry (ICP-MS) has been carried out and is reported in this paper. The results indicate that all geology units have LREE enrichment pattern, while a great difference exists between ΣREEs. For the total content of REEs in Qitianling Granite, the weathering crust has the highest level of ΣREEs with an average value of 605×10-6, and the limestone has the least ΣREEs with an average value of 154.3×10-6. In addition, the closer to the intrusions, the higher ΣREEs contents have in strata, even for the same lithology rock. In combination with REE-Y/ΣREE, ΣREE-δEu diagrams and Os Isotope tracer results, Qitianling granitoids might have mixed with some mantle materials. The content of REEs in the Qitianling Granite weathering crust (average value of RE2O3 is 814.8×10-6) are more than the cutoff grade of ion-absorbed-type REEs deposit (HREE RE2O3 0.05% and LREE 0.07%) in the main, which deserves further exploration.http://www.ykcs.ac.cn/cn/article/id/f761ec14-7dd7-454d-b16e-f885a3d03fa4qitianling intrusionbaishidu-feixianzhen geological profilerare earth elementsgeochemical characteristics |
spellingShingle | HE Han-han LI Jian-kang LI Chao SU Xiao-yun ZHAO Zhi ZHANG Yi-jun WANG Guo-rui Geochemical Characteristics of Rare Earth Elements in Deep Geological Profile of Qitianling Intrusion, Hunan Province Yankuang ceshi qitianling intrusion baishidu-feixianzhen geological profile rare earth elements geochemical characteristics |
title | Geochemical Characteristics of Rare Earth Elements in Deep Geological Profile of Qitianling Intrusion, Hunan Province |
title_full | Geochemical Characteristics of Rare Earth Elements in Deep Geological Profile of Qitianling Intrusion, Hunan Province |
title_fullStr | Geochemical Characteristics of Rare Earth Elements in Deep Geological Profile of Qitianling Intrusion, Hunan Province |
title_full_unstemmed | Geochemical Characteristics of Rare Earth Elements in Deep Geological Profile of Qitianling Intrusion, Hunan Province |
title_short | Geochemical Characteristics of Rare Earth Elements in Deep Geological Profile of Qitianling Intrusion, Hunan Province |
title_sort | geochemical characteristics of rare earth elements in deep geological profile of qitianling intrusion hunan province |
topic | qitianling intrusion baishidu-feixianzhen geological profile rare earth elements geochemical characteristics |
url | http://www.ykcs.ac.cn/cn/article/id/f761ec14-7dd7-454d-b16e-f885a3d03fa4 |
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