Nalaganje...
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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Main Authors: | , , |
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Format: | Artigo |
Jezik: | Inglês |
Izdano: |
MDPI AG
2020-02-01
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Serija: | Geosciences |
Teme: | |
Online dostop: | https://www.mdpi.com/2076-3263/10/2/56 |
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