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Global tectonic settings and deep mantle control on Hg and Au-Hg deposits Read chapter Read first chapter

2005 | OriginalPaper | Chapter

Geochemistry and gold content of the Triassic cabonaceous cherts of the Sikhote-Alin, Russia

Authors : Yu.G. Volokhin, A. I. Khanchuk, V. V. Ivanov, V. T. Kazachenko, V. V. Sattarova

Published in: Mineral Deposit Research: Meeting the Global Challenge

Publisher: Springer Berlin Heidelberg

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Triassic carbonaceous cherts are widesp-read in the Sikhote-Alin fold belt. They occur in a 4 to 20 m-thick sequence of interbedded cherts, carbonaceous cherts, and argillites that ranges in age from Upper Olenekian to Upper Anisian. The carbonaceous cherts are marine radiolarian rocks that contain 0.3 to 8.5 wt% C

org

. The majority of these rocks have undergone textural and mineralogical changes to a middle stage of catagenesis. Their organic matter contains low-grade oxidized humic acids with quinone, >CH

2

,-CH

3

hydrocarbon groups. The δ

13

C values are between −27.3 and −32.5 ‰. Carbonaceous cherts are anomalously enriched in V, B, Cu, Ni, Mo, Ag, and locally Au.

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previous chapter N2-Ar-He tracing systematics of ore-forming fluids: A case study from the Songxi large-scale Ag(Sb) deposit, eastern Guangdong Province, China
next chapter Genesis of PGE-polymetallic deposits in lower Cambrian black rock series, southern China: Evidence from fluid inclusion and inert gas isotopic studies
Metadata
Title
Geochemistry and gold content of the Triassic cabonaceous cherts of the Sikhote-Alin, Russia
Authors
Yu.G. Volokhin
A. I. Khanchuk
V. V. Ivanov
V. T. Kazachenko
V. V. Sattarova
Copyright Year
2005
Publisher
Springer Berlin Heidelberg
Book
Mineral Deposit Research: Meeting the Global Challenge

Print ISBN: 978-3-540-27945-7

Electronic ISBN: 978-3-540-27946-4

Copyright Year: 2005

DOI
https://doi.org/10.1007/3-540-27946-6_49