The DOI matches its Crossref record; 18 of the 18 references it cites were found in a registry or an index.
Isotopic evidence from the Ivrea Zone for a hybrid lower crust formed by magmatic underplating
Open accessAbstract
The large mafic complex overlying mantle peridotites in the Ivrea Zone of northern Italy originated by underplating of mantle-derived magma onto the base of continental crust, and may be a unique outcrop of typical mafic lower crust, sampled elsewhere only by mafic xenoliths. Neodymium and strontium isotope data show that the magmas assimilated large and roughly uniform proportions of crustal material. The resulting hybrid magmas have the same isotopic signature as, and may represent the lower-crustal 'roots' of, upper-crustal Hercynian granitoid intrusions.
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Citations
Cites
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Composition of the Continental Crust
Rudnick, R. L., & Gao, S. (2014) · Treatise on Geochemistry · doi:10.1016/b978-0-08-095975-7.00301-6 · Cited by 5,691
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Composition of the Continental Crust
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Chemical composition of the continental crust as revealed by studies in East China
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The persistent myth of crustal growth
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Metadata
- Authors
- Voshage, H., Hofmann, A. W., Mazzucchelli, M., Rivalenti, G., Sinigoi, S., Raczek, I., & Demarchi, G.
- Venue
- Nature
- Published
- 1990-10
- Volume
- 347
- Issue
- 6295
- Pages
- 731-736
- ISSN
- 0028-0836 (ISSN-L)
- 1476-4687
- OpenAlex
- W1995079291
- Cited by
- 302
- References
- 18
- FWCI
- 14.29
- Type
- journal article
- Language
- en
- Open access
- green
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- CoChat. (2026). Citation check: Isotopic evidence from the Ivrea Zone for a hybrid lower crust formed by magmatic underplating. https://app.cochat.ai/papers/10.1038/347731a0
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- Voshage, H., Hofmann, A. W., Mazzucchelli, M., Rivalenti, G., Sinigoi, S., Raczek, I., & Demarchi, G. (1990). Isotopic evidence from the Ivrea Zone for a hybrid lower crust formed by magmatic underplating. Nature. https://doi.org/10.1038/347731a0
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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
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