During the weathering of mineral deposits, trace elements are displaced from their original host minerals, are dispersed, and can subsequently occur in newly formed secondary phases in the regolith. In sedimentary cover, post-depositional weathering and diagenesis lead to the formation of a variety of secondary minerals. Of most interest are clay minerals, poorly crystalline minerals and Fe and M
The mobility of zinc in the regolith is important for several reasons, including the weathering of z...
International audienceThe distribution of four trace metals - nickel (Ni), chromium (Cr), manganese ...
At the present price of approximately US$600/troy oz, gold is clearly a valuable commodity. In order...
Geochemical dispersion of Au, base elements and their pathfinders is partly controlled by the availa...
SUMMARY. Classical clay mineralogy determinations and electron microprobe analyses of weathering min...
This chapter, like Churchman (2000), seeks to bring readers up to date with information and understa...
Metal anomalies in transported regolith that overlie bedrock-hosted mineralization indicate that a c...
weathering mantle is very thick, widespread, and, in many cases, capped by old and widely developed ...
International audienceREE, U and Th are often found as major elements in the same accessory minerals...
A body of komatiitic amphibolite, an enclave within the Archean high-grade orthogneisses in southern...
Western Australia, is difficult to explore due to structural complexity in the basement, a variably ...
© 1993 Damien LulofsRegolith profiles over and around zones of Pb-Zn mineralisation were investigate...
Weathering of sulphide minerals produces a large variety of Fe-oxide-bearing ochreous, varicoloured ...
Weathering destroys ome heavy minerals at the source so they are not represented in the resulting se...
The chemical and physical weathering of minerals is the fundamental process giving rise to much of t...
The mobility of zinc in the regolith is important for several reasons, including the weathering of z...
International audienceThe distribution of four trace metals - nickel (Ni), chromium (Cr), manganese ...
At the present price of approximately US$600/troy oz, gold is clearly a valuable commodity. In order...
Geochemical dispersion of Au, base elements and their pathfinders is partly controlled by the availa...
SUMMARY. Classical clay mineralogy determinations and electron microprobe analyses of weathering min...
This chapter, like Churchman (2000), seeks to bring readers up to date with information and understa...
Metal anomalies in transported regolith that overlie bedrock-hosted mineralization indicate that a c...
weathering mantle is very thick, widespread, and, in many cases, capped by old and widely developed ...
International audienceREE, U and Th are often found as major elements in the same accessory minerals...
A body of komatiitic amphibolite, an enclave within the Archean high-grade orthogneisses in southern...
Western Australia, is difficult to explore due to structural complexity in the basement, a variably ...
© 1993 Damien LulofsRegolith profiles over and around zones of Pb-Zn mineralisation were investigate...
Weathering of sulphide minerals produces a large variety of Fe-oxide-bearing ochreous, varicoloured ...
Weathering destroys ome heavy minerals at the source so they are not represented in the resulting se...
The chemical and physical weathering of minerals is the fundamental process giving rise to much of t...
The mobility of zinc in the regolith is important for several reasons, including the weathering of z...
International audienceThe distribution of four trace metals - nickel (Ni), chromium (Cr), manganese ...
At the present price of approximately US$600/troy oz, gold is clearly a valuable commodity. In order...
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