Strengths and limitations of zircon Lu-Hf and O isotopes in modelling crustal growth
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文摘

Juvenile addition to “hot zones” yields Lu-Hf arrays mimicking crustal reworking.

New zircon Hf-O isotope compilation indicates < 14% of Hf model ages are reliable.

Inverse modelling of global continental growth is limited by numerical artefacts.

Joint Hf-O modelling can provide improved constraints on crustal generation.

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