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Polymetallic mineralised veins in ferroan/A-type Cretaceous leucogranite, Stewart Island, New Zealand

AH AlliboneRodinian (NZ) Ltd, Wanaka, New ZealandCorrespondence[email protected]
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D MacKenzieDepartment of Geology, University of Otago, Dunedin, New ZealandView further author information

R TurnbullGNS Science, Dunedin, New ZealandView further author information

A TullochGNS Science, Dunedin, New ZealandView further author information

D CrawDepartment of Geology, University of Otago, Dunedin, New ZealandView further author information

M PalinDepartment of Geology, University of Otago, Dunedin, New ZealandView further author information

Supplemental material

Figure S2. Mineralogy, textures and paragenetic relationships within mineralized veins at North Red Head.

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Figure S1. Trace element characteristics of North Red Head leucogranite, mineralized veins, and altered rocks from throughout the North Red Head hydrothermal system.

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Table S2. Zircon analytical data collected on the LAICPMS facility at the University of Otago.

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Table S1. Full chemical analyses and summary descriptions of all samples discussed herein. Analytical methods noted in the table are described above. Elements and methods denoted n.d. were not determined.

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Polymetallic mineralised veins in ferroan/A-type Cretaceous leucogranite, Stewart Island, New Zealand

Figure S2. Mineralogy, textures and paragenetic relationships within mineralized veins at North Red Head.

Figure S1. Trace element characteristics of North Red Head leucogranite, mineralized veins, and altered rocks from throughout the North Red Head hydrothermal system.

Table S2. Zircon analytical data collected on the LAICPMS facility at the University of Otago.

Table S1. Full chemical analyses and summary descriptions of all samples discussed herein. Analytical methods noted in the table are described above. Elements and methods denoted n.d. were not determined.

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Polymetallic mineralised veins in ferroan/A-type Cretaceous leucogranite, Stewart Island, New Zealand

Figure S2. Mineralogy, textures and paragenetic relationships within mineralized veins at North Red Head.

Figure S1. Trace element characteristics of North Red Head leucogranite, mineralized veins, and altered rocks from throughout the North Red Head hydrothermal system.

Table S2. Zircon analytical data collected on the LAICPMS facility at the University of Otago.

Table S1. Full chemical analyses and summary descriptions of all samples discussed herein. Analytical methods noted in the table are described above. Elements and methods denoted n.d. were not determined.

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