Knott, Diane Clemens and Taylor, Hugh P., Jr. and Sinigoi, Silvano (1990) An oxygen isotope and chemical study of the Ivrea Zone, Italy: interaction between mafic magmas and lower crustal metamorphic rocks. Abstracts with Programs - Geological Society of America, 22 (7). p. 25. ISSN 0016-7592. https://resolver.caltech.edu/CaltechAUTHORS:20130820-104930829
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Abstract
The Ivrea Zone is arguably the best example of an exposed tectonic slice through middle to lowermost continental crust. The study area is dominated by a large, composite, ultramafic-mafic intrusion termed the Mafic Complex, which was emplaced during the late Hercynian (~260-300 Ma) into a middle amphibolite- to granulite-facies, metavolcanic-sedimentary sequence. Oxygen isotope analyses of ~130 samples from the Mafic Complex comprise the most complete data base presently available for underplated lower continental crust.
| Item Type: | Article |
|---|---|
| Additional Information: | © 1990 Geological Society of America. |
| Issue or Number: | 7 |
| Record Number: | CaltechAUTHORS:20130820-104930829 |
| Persistent URL: | https://resolver.caltech.edu/CaltechAUTHORS:20130820-104930829 |
| Usage Policy: | No commercial reproduction, distribution, display or performance rights in this work are provided. |
| ID Code: | 40735 |
| Collection: | CaltechAUTHORS |
| Deposited By: | Tony Diaz |
| Deposited On: | 27 Aug 2013 17:25 |
| Last Modified: | 03 Oct 2019 05:42 |
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