CoChat
Sign Up
Cited by 83High-pressure geophysics and materialsGeological and Geochemical AnalysisAstro and Planetary Science

Melting relations of peridotite and the density crossover in planetary mantles

Ohtani, Eiji, Nagata, Yoshihiko, Suzuki, Akio, Kato, Takumi·1995·Chemical Geology
DOI 10.1016/0009-2541(94)00139-y
Open this paper in CoChat — free account

Integrity signals

Registry

Crossref · 10.1016/0009-2541(94)00139-y

Cites

2 of 2 references verified0 citation errors · 0 not checkable

Statistics

Recomputing p-values needs the paper’s full text.

Claims the paper makes

We couldn’t retrieve this paper’s full text, so its claims and self-check weren’t run. The registry and citation checks still apply.

Claims other papers make about this one

Each is checked against this paper’s own text: does it say what the citing paper says it does?

  • High pressure in the mantle of a large rocky planet can prevent active volcanism at the surface by making melted rock negatively buoyant.

    “High pressure in the mantle of a large rocky planet can also prevent active volcanism at the surface by making melted rock negatively buoyant (Ohtani et al., 1995).”

    From The Astrobiology Primer v2.0 (2016) · cites this paper as Ohtani et al., 1995

Cites

Flagged first, then by citations

Cited by

Sorted by citations

  • The Astrobiology Primer v2.0

    Domagal-Goldman, S. D., Wright, K. E., Domagal-Goldman, S. D., Wright, K. E., Adamala, K., Arina de la Rubia, L., Bond, J., Dartnell, L. R., Goldman, A. D., Lynch, K., et al. (2016) · Astrobiology · doi:10.1089/ast.2015.1460 · Cited by 136 · see citing works

    “High pressure in the mantle of a large rocky planet can also prevent active volcanism at the surface by making melted rock negatively buoyant (Ohtani et al., 1995).”

Authors
Ohtani, E., Nagata, Y., Suzuki, A., & Kato, T.
Affiliations
  • Tohoku University (JP)
  • Ehime University (JP)
ORCID
Venue
Chemical Geology
Publisher
Elsevier BV
Published
1995-03
Volume
120
Issue
3-4
Pages
207-221
ISSN
0009-2541 (ISSN-L)
DOI
10.1016/0009-2541(94)00139-y
OpenAlex
W2005544172
Cited by
83
References
2
Citations by year
2026: 2 · 2025: 4 · 2024: 1 · 2023: 4 · 2022: 2 · 2021: 6 · 2020: 2 · 2019: 5 · 2018: 3 · 2017: 7 · 2016: 3 · 2014: 2 · 2013: 4 · 2012: 3
FWCI
2.52
Type
journal article
Language
en
Open access
closed
Licence
Locations
Chemical Geology (publishedVersion)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Geophysics › High-pressure geophysics and materials
  • Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
  • Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Astro and Planetary Science
Keywords
peridotite melting, Earth's mantle, majorite, olivine, compression curves, mantle diapirs, lunar mantle, Martian mantle, Martian meteorites, high-pressure melting

About these checks

Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.

Statistics and arithmetic are recomputed, not judged.

Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.

What counts as a claim ›How we measure confidence ›How we check this ›

Are you an author, or do you see a problem with this page? Request a review