Use of vegetation and soil in mineral exploration in areas of transported overburden, Yilgarn Craton, Western Australia: a contribution towards understanding metal transportation processes

被引:52
作者
Anand, R. R.
Cornelius, M.
Phang, C.
机构
[1] CRC LEME, CSIRO Exploration and Mining, Bentley, WA 6102
关键词
biogeochemistry; soil geochemistry; vegetation; metal migration mechanisms; Yilgarn Craton;
D O I
10.1144/1467-7873/07-142
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Five sites were selected in the semi-arid northern Yilgarn Craton (Jaguar VHMS Cu-Zn-Ag, Moolart Well An, Rumour An, Gossan Hill VHMS Cu-Zn-Au and McGrath North Au deposits) to test the use of vegetation as an exploration sampling medium in areas of transported overburden. A variety of vegetation samples (litter, roots, bark, branch wood and phyllodes) were collected from Mulga (Acacia aneura) plants. In addition, the soil from 10-20 cm below surface was sampled and analvsed following total, partial and selective digests to investigate any potential chemical signature of bedrock mineralization at surface. At all sites, selective extractions of the < 250 mu m fraction of soil show either no expression of buried mineralization or, where present, only a weak or ambiguous signature. In contrast, the vegetation survey shows a multi-element signature in different plant organs. Branches show very low anomaly contrasts or none at an. Phyllodes and bark generally show weak to moderate anomaly contrasts. Litter shows the greatest anomaly contrast of all plant material. There is also an enrichment in metals and an expression of the bedrock mineralization with good anomaly contrast in the uppermost soil horizon (0-4 cm) at Jaguar and this may indicate some mixing of litter and soil by bioturbation, and fixing on organic material, and Fe and/or Mn oxides. This contrasts with greater depths (10-20 cm) where no significant metal enrichment appears to have occurred, suggesting that most contained metals were fixed near-surface and do not percolate deeper into the profile. This is possibly due to slow decomposition of litter in and terrains, with continuous loss of soil an fine litter particles by wind erosion and bush fires. Our data support the hypothesis that vegetation plays an important role in bringing metals to surface in areas with a semi-arid to and climate and a low water-table.
引用
收藏
页码:267 / 288
页数:22
相关论文
共 97 条
[1]   Regolith geology of the Yilgarn Craton, Western Australia: implications for exploration [J].
Anand, RR ;
Paine, M .
AUSTRALIAN JOURNAL OF EARTH SCIENCES, 2002, 49 (01) :3-162
[2]  
ANAND RR, 2005, 22 INT GEOCH EXPL S, P27
[3]  
ANAND RR, 2003, YANDAL GOLD PROVINCE, P26
[4]  
[Anonymous], 3838 GEOL SURV CAN
[5]  
[Anonymous], EXPLOR NEWSL ASS APP
[6]  
[Anonymous], EARTH SCI J CHINA S
[7]  
[Anonymous], NOBLE METALS BIOL SY
[8]  
[Anonymous], DENV REG EXPL GEOL S
[9]  
APLIN TEH, 1975, W AUSTR YB, V14
[10]   Biogeochemistry of the Ballarat East Goldfield, Victoria, Australia [J].
Arne, DC ;
Stott, JE ;
Waldron, HM .
JOURNAL OF GEOCHEMICAL EXPLORATION, 1999, 67 (1-3) :1-14