Journal articles
Unravelling the root zone of ultramafic‐hosted black smokers‐like hydrothermalism from an Alpine analog
Abstract : Mid-Ocean Ridges host various types of hydrothermal systems including high-T black-smokers found in ultramafic rocks exhumed along slow spreading ridges. These systems are mostly described in two dimensions as their exposure on the present-day seafloor lacks the vertical dimension. One way to understand these systems at depth is to study their fossilized equivalents preserved on-land. Such observation can be done in the Platta nappe, Switzerland, where a Accepted Article This article is protected by copyright. All rights reserved Jurassic-aged mineralized system is exposed in 3D. Serpentinites host a Cu-Fe-Ni-Co-Zn-rich mineralization made of sulfides, magnetite and Fe-Ca-silicates either replacing serpentinites or within stockwork. Fe-Ca-silicates, abundant at the deepest levels, vanish in the mineralization close to the paleo-detachment. Fluids were channelized along mafic dykes and sills acting as preferential drains. Warm carbonation (~130°C) is the latest hydrothermal record. We propose that this system is an analog to the root zone of present-day serpentinite-hosted hydrothermal systems such as those found along the Mid-Atlantic Ridge.
Cited literature [16 references]
https://hal-insu.archives-ouvertes.fr/insu-02294388
Contributor : Isabelle Dubigeon Connect in order to contact the contributor
Submitted on : Monday, September 23, 2019 - 2:14:11 PM
Last modification on : Wednesday, November 17, 2021 - 12:33:16 PM
Long-term archiving on: : Sunday, February 9, 2020 - 7:47:13 AM
Contributor : Isabelle Dubigeon Connect in order to contact the contributor
Submitted on : Monday, September 23, 2019 - 2:14:11 PM
Last modification on : Wednesday, November 17, 2021 - 12:33:16 PM
Long-term archiving on: : Sunday, February 9, 2020 - 7:47:13 AM
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