Toco orogeny

The Toco orogeny was a mountain building affecting the rocks of northern Chile and northwestern Argentina during the Late Carboniferous and Permian. In 1991, researchers Bahlburg and Breitkurz noted that Chilean rocks had a 100 million lull magmatic and metamorphic "lull" from the Silurian to the Carboniferous. They defined the Toco orogeny as the period when active margin conditions returned in the region. ^[1]

References[edit]

^ Moreno, Teresa & Gibbons, Wes (2007). The Geology of Chile. The Geological Society. p. 5. ISBN 9781862392205.{{cite book}}: CS1 maint: multiple names: authors list (link)

[1] Moreno, Teresa & Gibbons, Wes (2007). The Geology of Chile. The Geological Society. p. 5. ISBN 9781862392205.{{cite book}}: CS1 maint: multiple names: authors list (link)

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Toco orogeny

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