Redox-controlled selenide mineralization in the upper old red sandstone

Samuel C. Spinks*, John Parnell, John W. Still

*Corresponding author for this work

Research output: Contribution to journalArticle

13 Citations (Scopus)

Abstract

Selenium concentrations occur in organic-rich lithologies such as coal, and as secondary accumulations from the oxidative mobilization, migration and subsequent concentration upon encountering reductants such as organic matter or H2S. Here we assess the redox mineralization of copper and lead selenide phases in the cores of reduction spheroids in Devonian sedimentary red beds. We propose that the selenide mineralization occurred as descending meteoric fluids, supplied with selenium from Carboniferous coal seams, migrated through a major fault plane into underlying sandstones where localized, microbially-induced reducing conditions prevailed. These findings and other occurrences of selenide mineralization between Devonian and Carboniferous strata on the British Isles suggest a widespread selenide mineralization system between strata of that age.

Original languageEnglish
Pages (from-to)173-182
Number of pages10
JournalScottish Journal of Geology
Volume50
Issue number2
Early online date3 Sep 2014
DOIs
Publication statusPublished - Oct 2014

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Old Red Sandstone
mineralization
selenium
red bed
fault plane
coal seam
mobilization
lithology
sandstone
coal
copper
organic matter
fluid

ASJC Scopus subject areas

  • Geology

Cite this

Redox-controlled selenide mineralization in the upper old red sandstone. / Spinks, Samuel C.; Parnell, John; Still, John W.

In: Scottish Journal of Geology, Vol. 50, No. 2, 10.2014, p. 173-182.

Research output: Contribution to journalArticle

Spinks, Samuel C. ; Parnell, John ; Still, John W. / Redox-controlled selenide mineralization in the upper old red sandstone. In: Scottish Journal of Geology. 2014 ; Vol. 50, No. 2. pp. 173-182.
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