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西澳Darling Range地区红土型铝土矿地球化学特征及源区研究

孙朋飞 江思宏 韩宁

地质学报2018,Vol.92Issue(3):587-603,17.
地质学报2018,Vol.92Issue(3):587-603,17.

西澳Darling Range地区红土型铝土矿地球化学特征及源区研究

Geochemical Characteristics and Source of the Laterite-type Bauxite Deposit in Darling Range, Western Australia

孙朋飞 1江思宏 2韩宁2

作者信息

  • 1. 中国地质大学(北京)地球科学与资源学院,北京,100083
  • 2. 国土资源部成矿作用与资源评价重点实验室,中国地质科学院矿产资源研究所,北京,100037
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摘要

Abstract

Located in western Australia,Darling Range is rich in laterite-type bauxite resources.In order to understand metallogenesis of the laterite-type bauxite in Darling Range and constrain the source of oreforming materials,this study carried out element geochemistry analysis and LA-ICP-MC dating of detrital zircons from bauxite and underlying granite.The results show that the bauxite in the Darling Range are composed mainly of Al2O3,Fe2O3,SiO2,and TiO2.Al2O3 has a negative relationship with SiO2,but a positive relationship with TiO2.It suggests that bauxite experienced the loss of Si and enrichment of A1 and Ti during the ore-forming process.Geochemical analysis shows that the bauxite is enriched in Th,U,Nb,Ta,Zr,Hf and Ti,and depleted in Ba,K,Sr,P and Sm.The bauxite is characterized by low REE contents from 1.36 × 10-6 to 65.58× 10-6,and the chondrite-normalized REE pattern slightly tilts to the right and shows enrichment in LREE.LA-ICP-MC detrital zircon U-Pb ages of the bauxite can be assigned to two groups:1167~1267 Ma (2 zircons) and 2539~2696 Ma (16 zircons).The former younger detrital zircons possibly came from Albany-Fraser orogeny,while the later older detrital zircons have the weighted average ages of 2579±15 Ma (MSWD=1.16),consistent with 2585±12 Ma (MSWD=0.83) of Archean granite,with the difference within the error.This indicates that besides the zircons from Archean granite,minor zircons in the laterite-type bauxite may derive from Albany-Fraser orogeny belt.Using Al2O3/TiO2 ratio,lgCr-lgNi plot,trace element ratios,and REE pattern to trace the source of laterite-type bauxite deposit,it can be concluded that Archean granite is the major source of ore-forming materials for the laterite-type bauxite deposit in the Darling Range of western Australia.

关键词

西澳/Darling Rang地区/铝土矿/U-Pb年代学/地球化学/源区研究

Key words

western Australia/Darling Range/bauxite/U-Pb geochronology/geochemistry/source

引用本文复制引用

孙朋飞,江思宏,韩宁..西澳Darling Range地区红土型铝土矿地球化学特征及源区研究[J].地质学报,2018,92(3):587-603,17.

基金项目

本文为国家地质大调查项目(编号1212011120325和121201103000150006)资助的成果. (编号1212011120325和121201103000150006)

地质学报

OA北大核心CSCDCSTPCD

0001-5717

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