Abstract
The schist-, sediment-, and intrusion-hosted Tertiary Au-Ag hydrothermal deposits of the northern Black Hills, South Dakota are localized and controlled by various types of fractures. This study is an attempt to distinguish between and discuss the possible causes of these fractures in three mines: Richmond Hill, Annie Creek - Foley Ridge (ACFR), and Gilt Edge. Five models based on the structural and tectonic settings of the northern Black Hills are proposed for the fracture origin. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 205-214 |
| Number of pages | 10 |
| Journal | Exploration & Mining Geology |
| Volume | 4 |
| Issue number | 3 |
| State | Published - 1995 |
ASJC Scopus subject areas
- Geotechnical Engineering and Engineering Geology
- Geology
Fingerprint
Dive into the research topics of 'Fracture control on the Tertiary epithermal-mesothermal gold deposits northern Black Hills, South Dakota'. Together they form a unique fingerprint.Cite this
- APA
- Author
- BIBTEX
- Harvard
- Standard
- RIS
- Vancouver