Abstract

Sedimentary uranium deposits, sulfur and phosphorus concentrated by organic matter in sediments, uranium stably transported from granite by aqueous solutions and deposited in reducing environment, dominant reducing agent in the environment not phosphorus abundance critical in determining whether ningyoite or uraninite is deposited, pyrite necessary as reducer and pH-regulator for genesis of ningyoite, Japan

First Page Preview

First page PDF preview
You do not currently have access to this article.