Abstract
Bedded barite deposits in northeastern Washington occur as distinct beds, from 1 to 45 feet thick, interbedded with quartz siltstones, argillites and limestone that may range in age from Ordovician to Carboniferous. Six of 9 known bedded barite deposits were selected for field and laboratory study. They are similar in many respects to other bedded and presumably marine sedimentary barite deposits in Nevada and Arkansas, including: 1) their conformity with the bedding of enclosing quartz siltstones, argillites and limestone, 2) their thin laminae (
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.
