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

Tavares Nassif, Miguel; Monecke, Thomas; Reynolds, T James; Kuiper, Yvette D; Goldfarb, Richard J; Piazolo, Sandra; Lowers, Heather A

Tavares Nassif, Miguel; Monecke, Thomas; Reynolds, T James; Kuiper, Yvette D; Goldfarb, Richard J; Piazolo, Sandra; Lowers, Heather A.

Afiliação

Tavares Nassif M; Department of Geology and Geological Engineering, Colorado School of Mines, Golden, CO, 80401, USA.
Monecke T; Department of Geology and Geological Engineering, Colorado School of Mines, Golden, CO, 80401, USA. tmonecke@mines.edu.
Reynolds TJ; Department of Geology and Geological Engineering, Colorado School of Mines, Golden, CO, 80401, USA.
Kuiper YD; FLUID INC., Denver, CO, 80202, USA.
Goldfarb RJ; Department of Geology and Geological Engineering, Colorado School of Mines, Golden, CO, 80401, USA.
Piazolo S; Department of Geology and Geological Engineering, Colorado School of Mines, Golden, CO, 80401, USA.
Lowers HA; Institute of Geophysics and Tectonics, University of Leeds, Leeds, LS2 9JT, UK.

Sci Rep ; 12(1): 17379, 2022 Oct 17.

Article em En | MEDLINE | ID: mdl-36253461

Texto completo

Imprimir

XML

PubMed Links

Buscar no Google

Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Idioma: En Revista: Sci Rep Ano de publicação: 2022 Tipo de documento: Article País de afiliação: Estados Unidos

Texto completo

Imprimir

XML

PubMed Links

Buscar no Google