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• W1963535120 abstract "Research Article| July 01, 2007 Fluid–Fluid Interactions in the Earth’s Lithosphere Axel Liebscher; Axel Liebscher Institute for Applied Geosciences, Technical University of Berlin, D-13355 Berlin, Germany, Department 4, Chemistry of the Earth, GeoForschungsZentrum Potsdam, Telegrafenberg, D-14473 Potsdam, Germany, axel.liebscher@tu-berlin.de Search for other works by this author on: GSW Google Scholar Christoph A. Heinrich Christoph A. Heinrich Isotope Geochemistry and Mineral Resources, Departement Erdwissenschaften NO, ETH Zentrum, CH-8092 Zurich, Switzerland, christoph.heinrich@erdw.ethz.ch Search for other works by this author on: GSW Google Scholar Author and Article Information Axel Liebscher Institute for Applied Geosciences, Technical University of Berlin, D-13355 Berlin, Germany, Department 4, Chemistry of the Earth, GeoForschungsZentrum Potsdam, Telegrafenberg, D-14473 Potsdam, Germany, axel.liebscher@tu-berlin.de Christoph A. Heinrich Isotope Geochemistry and Mineral Resources, Departement Erdwissenschaften NO, ETH Zentrum, CH-8092 Zurich, Switzerland, christoph.heinrich@erdw.ethz.ch Publisher: Mineralogical Society of America First Online: 09 Mar 2017 © The Mineralogical Society Of America Reviews in Mineralogy and Geochemistry (2007) 65 (1): 1–13. https://doi.org/10.2138/rmg.2007.65.1 Article history First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Axel Liebscher, Christoph A. Heinrich; Fluid–Fluid Interactions in the Earth’s Lithosphere. Reviews in Mineralogy and Geochemistry 2007;; 65 (1): 1–13. doi: https://doi.org/10.2138/rmg.2007.65.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyReviews in Mineralogy and Geochemistry Search Advanced Search Fluids rich in water, carbon and sulfur species and a variety of dissolved salts are a ubiquitous transport medium for heat and matter in the Earth’s interior. Fluid transport through the upper mantle and crust controls the origin of magmatism above subduction zones and results in natural risks of explosive volcanism. Fluids passing through rocks affect the chemical and heat budget of the global oceans, and can be utilized as a source of geothermal energy on land. Fluid transport is a key to the formation and the practical utilization of natural resources, from the origin of hydrothermal mineral deposits, through... You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W1963535120 title "Fluid Fluid Interactions in the Earth's Lithosphere" @default.
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