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The '''Rocas Verdes ophiolites''' are a series of [[greenschist]]s and other rocks forming constituting ophiolites in [[Magallanes Region]], southernmost Chile. The Rocas Verdes ophiolites represent the [[continental|continental]]-[[oceanic crust|oceanic]] crust that existed in the [[Magallanes Basin|Magallanes back-arc basin]] in the [[Mesozoic]].<ref>{{cite book |last=Stern |first=Charles R.|last2=De Wit |first2=Maarten J. |date=2013 |chapter=Rocas Verdes ophiolites, southernmost South America: remnants of progressive stages of development of oceanic-type crust in a continental margin back-arc basin |chapter-url=http://citeseerx.ist.psu.edu/viewdoc/download?doi=10.1.1.1026.5572&rep=rep1&type=pdf|editor-last=Dilek|editor-first=Y.|editor-last2=Robinson |editor-first2=P.T.|title=Ophiolites in Earth History |location= |publisher= |pages=665-683|series=Geological Society, London, Special Publications|issue=2018 |isbn= |author-link= }}</ref>
The '''Rocas Verdes ophiolites''' are a series of [[greenschist]]s and other rocks forming constituting ophiolites in [[Magallanes Region]], southernmost Chile. The Rocas Verdes ophiolites represent the [[continental crust|continental]]-[[oceanic crust|oceanic]] crust that existed in the [[Magallanes Basin|Magallanes back-arc basin]] in the [[Mesozoic]].<ref>{{cite book |last=Stern |first=Charles R.|last2=De Wit |first2=Maarten J. |date=2013 |chapter=Rocas Verdes ophiolites, southernmost South America: remnants of progressive stages of development of oceanic-type crust in a continental margin back-arc basin |chapter-url=http://citeseerx.ist.psu.edu/viewdoc/download?doi=10.1.1.1026.5572&rep=rep1&type=pdf|editor-last=Dilek|editor-first=Y.|editor-last2=Robinson |editor-first2=P.T.|title=Ophiolites in Earth History |location= |publisher= |pages=665-683|series=Geological Society, London, Special Publications|issue=2018 |isbn= |author-link= }}</ref>


==References==
==References==

Revision as of 02:02, 31 December 2018

The Rocas Verdes ophiolites are a series of greenschists and other rocks forming constituting ophiolites in Magallanes Region, southernmost Chile. The Rocas Verdes ophiolites represent the continental-oceanic crust that existed in the Magallanes back-arc basin in the Mesozoic.[1]

References

  1. ^ Stern, Charles R.; De Wit, Maarten J. (2013). "Rocas Verdes ophiolites, southernmost South America: remnants of progressive stages of development of oceanic-type crust in a continental margin back-arc basin". In Dilek, Y.; Robinson, P.T. (eds.). Ophiolites in Earth History. Geological Society, London, Special Publications. pp. 665–683.