A 400 Ma-long Nd-Hf isotopic evolution of melt-modified garnet-pyroxenites in an ancient subcontinental lithosphere (Lanzo North ophiolite, Western Alps)

Author:

Sanfilippo Alessio,Borghini Giulio,Guarnieri Luisa,Nakamura Eizo,Piccardo Giovanni B.,Vannucci Riccardo,Zanetti Alberto

Funder

Ministero dell'Istruzione dell'Universita e della Ricerca

Ministry of Education, Culture, Sports, Science and Technology

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference86 articles.

1. Re–Os and Lu–Hf isotopic constraints on the formation and age of mantle pyroxenites from the Bohemian Massif;Ackerman;Lithos,2016

2. Solar system abundances of the elements;Anders;Geochim. Cosmochim. Acta,1982

3. Plagioclase-facies thermobarometric evolution of the external Liguride pyroxenite-bearing mantle (Suvero, Italy);Basch;Ofioliti,2020

4. Highly siderophile element composition of the Earth’s primitive upper mantle: constraints from new data on peridotite massifs and xenoliths;Becker;Geochim. Cosmochim. Acta,2006

5. Hf–Nd isotope decoupling in the oceanic lithosphere. Constraints from spinel peridotites from Oahu, Hawaii;Bizimis;Earth Planet. Sci. Lett.,2003

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