"The general geology is briefly described, together with the available factual data regarding the nature and origin of the lenticular gold quartz veins. These are abundant throughout the region, and their structure and simple mineralogy indicates that they are of the deep zone type. It is concluded that the mineralization is genetically related to a widespread invasion of the region by alaskite." The veins occur in complex pre-Cambrian igneous rocks.

This content is PDF only. Please click on the PDF icon to access.

First Page Preview

First page PDF preview
You do not have access to this content, please speak to your institutional administrator if you feel you should have access.