Provenance of detrital pyrite in Archean sedimentary rocks: Examples from the Witwatersrand Basin

Detrital pyrite is an accessory mineral in clastic sedimentary rocks deposited prior to c. 2.4 Ga. It is a redox-sensitive mineral and an indicator of low oxygen levels prior to the rise of atmospheric oxygen in the early Paleoproterozoic. Resistance to mechanical abrasion, availability in Archean s...

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Main Authors: da Costa, G., Hofmann, A., Agangi, Andrea
Format: Book Chapter
Published: Elsevier 2016
Online Access:http://hdl.handle.net/20.500.11937/36531
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author da Costa, G.
Hofmann, A.
Agangi, Andrea
author_facet da Costa, G.
Hofmann, A.
Agangi, Andrea
author_sort da Costa, G.
building Curtin Institutional Repository
collection Online Access
description Detrital pyrite is an accessory mineral in clastic sedimentary rocks deposited prior to c. 2.4 Ga. It is a redox-sensitive mineral and an indicator of low oxygen levels prior to the rise of atmospheric oxygen in the early Paleoproterozoic. Resistance to mechanical abrasion, availability in Archean source rocks, and high density make it a common component of Archean quartz pebble conglomerates, some of which may be gold-bearing. The provenance of pyrite may include sediments and sedimentary rock successions, volcanogenic or sedimentary exhalative massive sulfide deposits, magmatic-hydrothermal deposits, and igneous rocks. The morphology and texture of pyrite grains, the nature of mineral inclusions, trace element geochemistry, and isotopic composition as well as age are the main variables that can be used to evaluate their source. In the Mesoarchean Witwatersrand Basin of South Africa, the world's largest gold deposit, detrital pyrite is mainly derived from sedimentary sources and synsedimentary precipitates.
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spelling curtin-20.500.11937-365312017-09-13T15:29:12Z Provenance of detrital pyrite in Archean sedimentary rocks: Examples from the Witwatersrand Basin da Costa, G. Hofmann, A. Agangi, Andrea Detrital pyrite is an accessory mineral in clastic sedimentary rocks deposited prior to c. 2.4 Ga. It is a redox-sensitive mineral and an indicator of low oxygen levels prior to the rise of atmospheric oxygen in the early Paleoproterozoic. Resistance to mechanical abrasion, availability in Archean source rocks, and high density make it a common component of Archean quartz pebble conglomerates, some of which may be gold-bearing. The provenance of pyrite may include sediments and sedimentary rock successions, volcanogenic or sedimentary exhalative massive sulfide deposits, magmatic-hydrothermal deposits, and igneous rocks. The morphology and texture of pyrite grains, the nature of mineral inclusions, trace element geochemistry, and isotopic composition as well as age are the main variables that can be used to evaluate their source. In the Mesoarchean Witwatersrand Basin of South Africa, the world's largest gold deposit, detrital pyrite is mainly derived from sedimentary sources and synsedimentary precipitates. 2016 Book Chapter http://hdl.handle.net/20.500.11937/36531 10.1016/B978-0-12-803386-9.00018-6 Elsevier restricted
spellingShingle da Costa, G.
Hofmann, A.
Agangi, Andrea
Provenance of detrital pyrite in Archean sedimentary rocks: Examples from the Witwatersrand Basin
title Provenance of detrital pyrite in Archean sedimentary rocks: Examples from the Witwatersrand Basin
title_full Provenance of detrital pyrite in Archean sedimentary rocks: Examples from the Witwatersrand Basin
title_fullStr Provenance of detrital pyrite in Archean sedimentary rocks: Examples from the Witwatersrand Basin
title_full_unstemmed Provenance of detrital pyrite in Archean sedimentary rocks: Examples from the Witwatersrand Basin
title_short Provenance of detrital pyrite in Archean sedimentary rocks: Examples from the Witwatersrand Basin
title_sort provenance of detrital pyrite in archean sedimentary rocks: examples from the witwatersrand basin
url http://hdl.handle.net/20.500.11937/36531