Abstract
Research Article| January 01, 2008 Fluid Inclusion Thermobarometry as a Tracer for Magmatic Processes Thor H. Hansteen; Thor H. Hansteen IFM-GEOMAR, Leibniz-Institute for Marine Sciences, Dynamics of the Ocean Floor, D-24148 Kiel, Germany, thansteen@ifm-geomar.de Search for other works by this author on: GSW Google Scholar Andreas Klügel Andreas Klügel Fachbereich Geowissenschaften, Universität Bremen, D-28334 Bremen, Germany, akluegel@uni-bremen.de Search for other works by this author on: GSW Google Scholar Author and Article Information Thor H. Hansteen IFM-GEOMAR, Leibniz-Institute for Marine Sciences, Dynamics of the Ocean Floor, D-24148 Kiel, Germany, thansteen@ifm-geomar.de Andreas Klügel Fachbereich Geowissenschaften, Universität Bremen, D-28334 Bremen, Germany, akluegel@uni-bremen.de Publisher: Mineralogical Society of America First Online: 13 Jul 2017 © The Mineralogical Society Of America Reviews in Mineralogy and Geochemistry (2008) 69 (1): 143–177. https://doi.org/10.2138/rmg.2008.69.5 Article history First Online: 13 Jul 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Thor H. Hansteen, Andreas Klügel; Fluid Inclusion Thermobarometry as a Tracer for Magmatic Processes. Reviews in Mineralogy and Geochemistry 2008;; 69 (1): 143–177. doi: https://doi.org/10.2138/rmg.2008.69.5 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 Fluid inclusions in minerals may form in any type of volcanic or plutonic rock ranging from mafic to silicic compositions. Because all igneous rocks reach fluid saturation at some stage during their evolution, fluids trapped as inclusions in magmatic minerals belong to a certain paragenesis or phase assemblage, which may include minerals, melts and one or more fluid phases. These fluid inclusions reflect one or more stages during rock evolution, and can be used to constrain multistage formation and evolution processes including ascent histories, magma chamber processes and crystallization behavior. Fluid inclusions can provide thermobarometric data on various timescales. During... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
Published Version
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
