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pro vyhledávání: '"Mihai Ducea"'
Trace elements in zircon are a promising proxy to quantitatively study long-term Earth’s lithospheric processes and its geodynamic regimes. The zircon Eu anomaly reflects the crystallization environment of its felsic or intermediate parental magma.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5002c309c4bbdec3176a01a95d59d6dd
https://doi.org/10.5194/egusphere-egu23-1954
https://doi.org/10.5194/egusphere-egu23-1954
Autor:
Peter Luffi, Mihai Ducea
Publikováno v:
Eos. 103
The chemical composition of orogenic igneous rocks and their zircons is sensitive to crustal thickness and can be used to quantify the evolution of Moho depths beneath continents back in time.
Publikováno v:
Goldschmidt2022 abstracts.
Autor:
Lőrincz Sarolta, Melinte-Dobrinescu Mihaela, Relu Roban, Mihai Ducea, Valentina Cetean, Marian Munteanu, Vlad-Victor Ene
Publikováno v:
Goldschmidt2022 abstracts.
Autor:
Peter Luffi, Mihai Ducea
Publikováno v:
Reviews of geophysics (Washington, D.C. : 1985). 60(2)
Convergent plate boundaries are key sites for continental crustal formation and recycling. Quantifying the evolution of crustal thickness and paleoelevation along ancient convergent margins represents a major goal in orogenic system analyses. Chemica
Publikováno v:
Goldschmidt Abstracts.
Publikováno v:
Goldschmidt Abstracts.
Autor:
BRADLEY HACKER, PETER LUFFI, VALERY LUTKOV, VLADISLAV MINAEV, LOTHAR RATSCHBACHER, TERRY PLANK, MIHAI DUCEA, ALBERTO PATIO-DOUCE, MICHAEL McWILLIAMS, JIM METCALF
Publikováno v:
Journal of Petrology; Aug2005, Vol. 46 Issue 8, p1661-1687, 27p