Abstract
Measurements have been made on fluid inclusions from mines and drill core within and adjacent to the Viburnum Trend and Northern Arkansas Zinc Mississippi Valley-type districts. Hydrothermal dolomite is the primary host mineral for the inclusions examined, but measurements have also been made on inclusions in sphalerite and calcite. Measurements of homogenization temperature (Th) and final melting temperature of ice (Tm) for 306 fluid inclusions are tabulated and briefly discussed. Results of this study give information on temperature and salinity of the ore fluids beyond the boundaries of the mining districts and provide insight into the regional distribution of the hot, saline brines trapped in the inclusions.
Sign-in/Register to access full text options 
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.
