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Geochronology and Stable Isotope Analysis of Fracture-Fill and Karst Mineralization Reveal Sub-Surface Paleo-Fluid Flow and Microbial Activity of the COSC-1 Borehole, Scandinavian Caledonides

The deep biosphere hosted in fractured rocks within the upper continental crust is one of the least understood and studied ecological realms on Earth. Scarce knowledge of ancient life and paleo-fluid flow within this realm is owing to the lack of deep drilling into the crust. Here we apply microscal...

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Bibliografske podrobnosti
Main Authors: Henrik Drake, Nick M. W. Roberts, Martin J. Whitehouse
Format: Artigo
Jezik:Inglês
Izdano: MDPI AG 2020-02-01
Serija:Geosciences
Teme:
Online dostop:https://www.mdpi.com/2076-3263/10/2/56
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