2014
DOI: 10.1016/j.epsl.2013.12.029
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Hafnium isotopes and Zr/Hf of rutile and zircon from lower crustal metapelites (Ivrea–Verbano Zone, Italy): Implications for chemical differentiation of the crust

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Cited by 40 publications
(19 citation statements)
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“…(2018), local occurrences of granulite‐facies metapelites ( V p = 6.3–7.2 km s −1 , V s = 3.8–4.1 km s −1 ; Weiss et al., 1999; Khazenehdari et al., 2000). North of the Po Plain, similar granulite facies metapelites are also exposed at Earth's surface (e.g., Ewing et al., 2014). In the region labeled as ALC 1 (Figure 6c), the locally high V p / V s ratios >1.8 associated to V p ∼7.0–7.3 km s −1 may be interpreted as gabbro underplated at the base of the Adriatic lower crust.…”
Section: Absolute Velocity Structure Of the Crust And The Mantle Wedgementioning
confidence: 99%
“…(2018), local occurrences of granulite‐facies metapelites ( V p = 6.3–7.2 km s −1 , V s = 3.8–4.1 km s −1 ; Weiss et al., 1999; Khazenehdari et al., 2000). North of the Po Plain, similar granulite facies metapelites are also exposed at Earth's surface (e.g., Ewing et al., 2014). In the region labeled as ALC 1 (Figure 6c), the locally high V p / V s ratios >1.8 associated to V p ∼7.0–7.3 km s −1 may be interpreted as gabbro underplated at the base of the Adriatic lower crust.…”
Section: Absolute Velocity Structure Of the Crust And The Mantle Wedgementioning
confidence: 99%
“…Atom probe specimens (1–8) were prepared from two ~200 µ m grains of the WHQ rutile reference material (Clark et al, 2000) mounted in epoxy. The rutile has a 207 Pb/ 206 Pb thermal ionization mass spectrometry (TIMS) age of 2642 Ma (precision not quoted) (Ewing, 2011, and references therein). The rutile is ~99 wt% TiO 2 with Cr (10,643 ± 3,227 µ g/g) and V (1,355 ± 748 µ g/g) (Ewing, 2011, and references therein).…”
Section: Sample Descriptionmentioning
confidence: 99%
“…The rutile has a 207 Pb/ 206 Pb thermal ionization mass spectrometry (TIMS) age of 2642 Ma (precision not quoted) (Ewing, 2011, and references therein). The rutile is ~99 wt% TiO 2 with Cr (10,643 ± 3,227 µ g/g) and V (1,355 ± 748 µ g/g) (Ewing, 2011, and references therein). The presence of these elements is of great importance as both have the potential for isotopic interference with Ti and with trace elements of interest—e.g.…”
Section: Sample Descriptionmentioning
confidence: 99%
“…, Ewing et al . ). Due to its preference for high field‐strength elements, rutile has found applications in provenance studies where the Cr/Nb ratio is suggested to indicate a metabasic or metapelitic origin (e.g., Zack et al .…”
mentioning
confidence: 97%