Abstract
The Beishan orogenic belt is located in the south rim of central Asia orogenic belt, the intersection of east Tianshan and Tarim plates. Thus, the geological structure is extremely complex. The gold deposits are widely distributed in various types and the met allogenic mechanism is complex. Overall, the gold deposits in Beishan orogenic belt are mostly developed in Palaeozoic continental plate collision and butting belt, which has a certain spatial and temporal distribution law. Huaniushan gold deposit is a typical gold deposit in Beishan Orogenic belt. This paper carried out a detailed study of the geology of Huaniushan gold deposit, to provide some basis for the classification of met allogenic stage.
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 callMore From: IOP Conference Series: Earth and Environmental Science
Disclaimer: 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.
