Gold: A tracer of the dynamics of tropical laterites

Fabrice Colin, Zakaria Sanfo, Erick Brown, Didier Bourlès, Ambroise Edou Minko

Research output: Contribution to journalArticlepeer-review

2 Scopus citations

Abstract

Lareites have developed essentially from long-term exposure of cratonal rocks to the atmosphere and hydrosphere. The properties of gold (density and relative insolubility) make residual gold parrticles tracers of surficial processes causing mineralized laterites. Gold particles are useful in distinguishing between in situ chemical weathering and physical transport on African lateritic systems developed on slowly eroding stble landforms. In an equatorial rainforest setting, chemical dissolution and translocation of fine particles are the dominant processes. Episodic alluvial and/or colluvial transport appears to contribute to laterite formation in the subsahelian steppe. The use of gold particles, coupled with the examination of in situ 10Be from auriferous quartz, indicates the applicability of such methods for examination of laritic weathering dynamics of the tropical "transcontinental" lithosphere.

Original languageEnglish (US)
Pages (from-to)81-84
Number of pages4
JournalGeology
Volume25
Issue number1
DOIs
StatePublished - Jan 1997
Externally publishedYes

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