Water table movement and supergene enrichment at Spence porphyry copper deposit,northern Chile

Abstract

Get full access to this article

View all access options for this article.

References

Ague

, Brimhall

GH.

1989. Geochemical modeling of steady state fluid flow and chemical reaction during supergene enrichment of porphyry copper deposits. Econ Geol. 84(3):506–528. doi: 10.2113/gsecongeo.84.3.506

Clarke

JDA.

2006. Antiquity of aridity in the Chilean Atacama Desert. Geomorphology. 73(1–2):101–114. doi: 10.1016/j.geomorph.2005.06.008

Cooper

, Adams

, Blundy

, Farley

, McKeon

, Ruggiero

2016. Aridity-induced Miocene canyon incision in the Central Andes. Geol. 44(8):675–678. doi: 10.1130/G38254.1

Rowland

, Clark

AH.

2001. GSA annual meeting abstract.

Rye

, Bethke

, Wasserman

MD.

1992. The stable isotope geochemistry of acid sulfate alteration. Econ Geol. 87(2):225–262. doi: 10.2113/gsecongeo.87.2.225

Sillitoe

RH.

2005. Econ Geol. 100th Anniversary Vol.: 723–768.

Sillitoe

, McKee

EH.

1996. Age of supergene oxidation and enrichment in the Chilean porphyry copper province. Econ Geol. 91(1):164–179. doi: 10.2113/gsecongeo.91.1.164