Formation of orogenic gold deposits by progressive movement of a fault-fracture mesh through the upper crustal brittle-ductile transition zone.

Saved in:
Bibliographic Details
Title: Formation of orogenic gold deposits by progressive movement of a fault-fracture mesh through the upper crustal brittle-ductile transition zone.
Authors: Tavares Nassif, Miguel1 (AUTHOR), Monecke, Thomas1 (AUTHOR) tmonecke@mines.edu, Reynolds, T. James1,2 (AUTHOR), Kuiper, Yvette D.1 (AUTHOR), Goldfarb, Richard J.1 (AUTHOR), Piazolo, Sandra3 (AUTHOR), Lowers, Heather A.4 (AUTHOR)
Source: Scientific Reports. 10/17/2022, Vol. 12 Issue 1, p1-11. 11p.
Database: Academic Search Ultimate
Full text is not displayed to guests.
Description
ISSN:20452322
DOI:10.1038/s41598-022-22393-9