| Article ID | Journal | Published Year | Pages | File Type | 
|---|---|---|---|---|
| 4697555 | Ore Geology Reviews | 2013 | 16 Pages | 
Abstract
												⺠The tectonic regime is confirmed as major factor in controlling mineralization style. ⺠Porphyry emplacement is confirmed as occurring at the end of an orogeny. ⺠Strain fabrics help to discriminate deposits placed under different tectonic settings. ⺠Strain fabrics help to identify stages during the hydrothermal system evolution.
											Keywords
												
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											Authors
												MarÃa S. Japas, Nora A. Rubinstein, Laura E. Kleiman, 
											