Typical features of metallogenic provinces

Abstract

Other| December 01, 1965 Typical features of metallogenic provinces Walther E. Petrascheck Walther E. Petrascheck Search for other works by this author on: GSW Google Scholar Author and Article Information Walther E. Petrascheck Publisher: Society of Economic Geologists First Online: 02 Mar 2017 Online ISSN: 1554-0774 Print ISSN: 0361-0128 GeoRef, Copyright 2008, American Geological Institute. Reference includes data from Bibliography and Index of North American Geology, U. S. Geological Survey, Reston, VA, United States Economic Geology (1965) 60 (8): 1620–1634. https://doi.org/10.2113/gsecongeo.60.8.1620 Article history First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Walther E. Petrascheck; Typical features of metallogenic provinces. Economic Geology 1965;; 60 (8): 1620–1634. doi: https://doi.org/10.2113/gsecongeo.60.8.1620 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyEconomic Geology Search Advanced Search Abstract 'A metallogenic province is the entity of mineral deposits that formed during a tectonic-metallogenic epoch within a major tectonic unit and which are characterized by related mineral composition, form of the deposits, and intensity of mineralization.' The concept of a metallogenic province is reviewed in terms of the following topics: regional-tectonic types of ore-bearing provinces; evolution of provinces in time; composition of ores characterizing the provinces; the form of ore deposits in individual provinces; density of mineralization. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.