The U.S. Midcontinent: a new frontier for mineral exploration.
Episodes
By: W. P. Pratt and P.K. Sims
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Abstract
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
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | The U.S. Midcontinent: a new frontier for mineral exploration. |
| Series title | Episodes |
| Volume | 10 |
| Issue | 4 |
| Year Published | 1987 |
| Language | English |
| Larger Work Type | Article |
| Larger Work Subtype | Journal Article |
| Larger Work Title | Episodes |
| First page | 303 |
| Last page | 307 |