超基性岩红土风化壳中REE地球化学：不同气候风化剖面的对比

付伟; 黄小荣; 杨梦力; 雷良奇; 牛虎杰; 张亚倩

doi:10.3799/dqkx.2014.067

Volume 39 Issue 6

Jun. 2014

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Article Navigation > Earth Science > 2014 > 39(6): 716-732

Fu Wei, Huang Xiaorong, Yang Mengli, Lei Liangqi, Niu Hujie, Zhang Yaqian, 2014. REE Geochemistry in the Laterite Crusts Derived from Ultramafic Rocks: Comparative Study of Two Laterite Profiles under Different Climate Condition. Earth Science, 39(6): 716-732. doi: 10.3799/dqkx.2014.067

Citation:

Fu Wei, Huang Xiaorong, Yang Mengli, Lei Liangqi, Niu Hujie, Zhang Yaqian, 2014. REE Geochemistry in the Laterite Crusts Derived from Ultramafic Rocks: Comparative Study of Two Laterite Profiles under Different Climate Condition. Earth Science, 39(6): 716-732. doi: 10.3799/dqkx.2014.067

Citation:

Fu Wei, Huang Xiaorong, Yang Mengli, Lei Liangqi, Niu Hujie, Zhang Yaqian, 2014. REE Geochemistry in the Laterite Crusts Derived from Ultramafic Rocks: Comparative Study of Two Laterite Profiles under Different Climate Condition. Earth Science, 39(6): 716-732. doi: 10.3799/dqkx.2014.067

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REE Geochemistry in the Laterite Crusts Derived from Ultramafic Rocks: Comparative Study of Two Laterite Profiles under Different Climate Condition

doi: 10.3799/dqkx.2014.067

Fu Wei^{1, 2, 3
,},
Huang Xiaorong³,
Yang Mengli³,
Lei Liangqi^{1, 2, 3},
Niu Hujie⁴,
Zhang Yaqian³

1.
Guangxi Experiment Center of Mining, Metallurgy and Environmental Sciences, Guilin University of Technology, Guilin 541004, China
2.
Guangxi Key Laboratory of Hidden Metallic Ore Deposits Exploration, Guilin University of Technology, Guilin 541004, China
3.
College of Earth Sciences, Guilin University of Technology, Guilin 541004, China
4.
Jinchuan Group Co., Ltd., Jinchang 737100, China

Received Date: 2013-12-01
Publish Date: 2014-06-15

Abstract

Abstract

To understand the characteristics and evolution of REE during the process of the ultramafic laterization under different climate conditions, two outcrops Kolonodale in Indonesia and Yuanjiang in China are chosen for comparision. It is found that the contents of REE from the laterite crusts are higher than those from the bed rocks in both places (enrichment factor being 44.21 and 236.19 respectively).The indices of differentiation between the LREE and HREE decrease with profile downward toward, and the indice of Ce anomaly shows a shift from the positive Ce anomaly in the upper segment to negative Ce anomaly in the lower part. The difference between the two profiles lies in the distribution of the highest REE enriched segment. The laterite layer represent the most REE enriched for the Yuanjiang, whereas the saprolite layer for the Kolonodale. The evaluation of the mass balance shows remarkable migration and differentiation of REE in the ultramafic laterization process, which were constrained effectively by the pH environmentand organic matter (O.M.). The results indicate that climate have had great influence on the geochemical evolution of REE during the ultramafic laterization. Under the rainforest climate condition, the REE from the Kolonodale originates mainly from the basal rocks and has experienced intensive redistribution during the laterization; whereas the REE from the Yuanjiang has a mixed source stemming from both the parent rock and aeolian sediment, and it has been through only slight redistribution during the laterization.
- rare earth element,
- laterite crust,
- ultramafic rock,
- climate condition,
- geochemistry

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References(102)

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REE Geochemistry in the Laterite Crusts Derived from Ultramafic Rocks: Comparative Study of Two Laterite Profiles under Different Climate Condition

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