The U.S. Midcontinent: a new frontier for mineral exploration.
January 1, 1987
The north-central US Midcontinent is underlain by a considerable thickness of sedimentary rocks, mostly Paleozoic, which lie upon a heterogeneous basement of Precambrian granitoid and metamorphic rocks. This article describes a representative sample of Midcontinent geology and explains why the authors believe this region is a 'new frontier' for mineral exploration and discovery. -Authors
Citation Information
| Publication Year | 1987 |
|---|---|
| Title | The U.S. Midcontinent: a new frontier for mineral exploration. |
| Authors | W. P. Pratt, P.K. Sims |
| Publication Type | Article |
| Publication Subtype | Journal Article |
| Series Title | Episodes |
| Index ID | 70014743 |
| Record Source | USGS Publications Warehouse |