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Cited by 1,451

The DOI matches its Crossref record; 38 of the 38 references it cites were found in a registry or an index.

Magmatic and Crustal Differentiation History of Granitic Rocks from Hf-O Isotopes in Zircon

Kemp, A. I. S., Hawkesworth, C. J., Foster, G. L., Paterson, B. A., Woodhead, J. D., Hergt, J. M., Gray, C. M., Whitehouse, M. J.·2007·Science

Abstract

Granitic plutonism is the principal agent of crustal differentiation, but linking granite emplacement to crust formation requires knowledge of the magmatic evolution, which is notoriously difficult to reconstruct from bulk rock compositions. We unlocked the plutonic archive through hafnium (Hf) and oxygen (O) isotope analysis of zoned zircon crystals from the classic hornblende-bearing (I-type) granites of eastern Australia. This granite type forms by the reworking of sedimentary materials by mantle-like magmas instead of by remelting ancient metamorphosed igneous rocks as widely believed. I-type magmatism thus drives the coupled growth and differentiation of continental crust.

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Metadata

Authors
Kemp, A. I. S., Hawkesworth, C. J., Foster, G. L., Paterson, B. A., Woodhead, J. D., Hergt, J. M., Gray, C. M., & Whitehouse, M. J.
Venue
Science
Published
2007-02-16
Volume
315
Issue
5814
Pages
980-983
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W2086557360
Cited by
1,451
References
38
FWCI
22.13
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Magmatic and Crustal Differentiation History of Granitic Rocks from Hf-O Isotopes in Zircon. https://app.cochat.ai/papers/10.1126/science.1136154
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Kemp, A. I. S., Hawkesworth, C. J., Foster, G. L., Paterson, B. A., Woodhead, J. D., Hergt, J. M., Gray, C. M., & Whitehouse, M. J. (2007). Magmatic and Crustal Differentiation History of Granitic Rocks from Hf-O Isotopes in Zircon. Science. https://doi.org/10.1126/science.1136154

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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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