Skip to Main Content
Skip Nav Destination

Disseminations of the ore minerals in clastic sedimentary rocks characterize this deposit type. Deposits occur in marine, paralic, lacustrine, and continental host rocks at or near a redox boundary. Three subtypes are distinguished on the basis of the major, economically-viable commodity and on the relation to the redox boundary. Sandstone uranium (8.1) and sandstone lead (8.2) deposits are associated with reductants within porous oxidizing sandstones; sedimenthosted stratiform copper (8.3) deposits occur in reduced host rocks adjacent to redbeds.

You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
Close Modal

or Create an Account

Close Modal
Close Modal