Refference : The 25th Symposium on Geoscience;Tehran
Publishing Year : 1385

Abstract :

Study area is located in south of Mashhad city and into Binaloud structure zone. Main structural mien in district is faults which Most of this trended NW-SE and is thrust type and activity of some this fault show with movement beds of Miocene sediment (and Quaternary). Mineralization zone of metals element most are in form vein and veinlet, by closing relationship which shown characteristic features of open space filling texture. Generally country rocks of these veins are carbonate rocks (Paleozoic). Abundant of iron oxide, silicification, dolomitization in mineralization zone to suggest is present and effect hydrothermal fluids in forming alteration and mineralization. Result of chemical analyze shown average valuable element such as Fe, Ba, Cu, Sb, As is high, also high grade and anomaly of Sn, Ag is astringency to attention. Geology setting, historical documents and finding old mining work in study area was encourage for tin mineralization.

Subject List : Mineralization