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Cited by 302

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 access
Voshage, H., Hofmann, A. W., Mazzucchelli, M., Rivalenti, G., Sinigoi, S., Raczek, I., Demarchi, G.·1990·Nature

Abstract

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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Crossref · 10.1038/347731a0

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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
The paper
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).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.