2022
DOI: 10.1029/2022gc010472
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Compositional Data Analysis (CoDA) of Clinopyroxene From Abyssal Peridotites

Abstract: Mid-ocean ridges are a major source of crust-mantle differentiation on Earth, through the processes of partial melting, melt transport and reaction, and fractional crystallization in the crust and uppermost mantle (Kelemen et al., 1997). Abyssal peridotites provide direct samples of oceanic upper mantle and are important for understanding mantle chemistry and how oceanic lithosphere develops (e.g.,

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Cited by 4 publications
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“…Because these peridotites lack clinopyroxene, which is generally the main budget of incompatible trace elements in peridotites, it is difficult to obtain their mineral trace elements compositions. However, recent studies show that trace element compositions of olivine and orthopyroxene do in fact record the formation and later metasomatic/metamorphic processes (e.g., Demouchy & Alard, 2021; Jean & Shervais, 2017; Nishio et al., 2022a; Scott et al., 2016). In this study, we examine olivine and orthopyroxene trace element compositions in addition to the petrography and mineral major element compositions from one of the clinopyroxene‐free ultra‐depleted peridotite bodies from the Kamuikotan unit.…”
Section: Introductionmentioning
confidence: 99%
“…Because these peridotites lack clinopyroxene, which is generally the main budget of incompatible trace elements in peridotites, it is difficult to obtain their mineral trace elements compositions. However, recent studies show that trace element compositions of olivine and orthopyroxene do in fact record the formation and later metasomatic/metamorphic processes (e.g., Demouchy & Alard, 2021; Jean & Shervais, 2017; Nishio et al., 2022a; Scott et al., 2016). In this study, we examine olivine and orthopyroxene trace element compositions in addition to the petrography and mineral major element compositions from one of the clinopyroxene‐free ultra‐depleted peridotite bodies from the Kamuikotan unit.…”
Section: Introductionmentioning
confidence: 99%