Abstract
Through mass change calculation of the bauxite in the Wuchuan-Zheng, an-Daozhen (WZD) area to reveal the migration regular of elements in the ore-forming process: major elements all have loss except aluminum element which keep steady in the ore-forming process of the WZD bauxite deposit; Major elements in the upper and middle part of the profile have a large scale of runoff, in the lower part of the profile just have a small scale of runoff, and some elements concentrated in the lower part of the profile, above all of these shows that major elements have a downward moving trend. Alkaline metal have the largest scale of runoff demonstrated that the ore-forming environment is acidic.
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.
