Whole-rock major and trace element compositions of peridotite and mafic rock samples from the Horoman Peridotite Complex, Japan. Major elements and Sc, V, Cr, Co, and Ni were measured by XRF and the other trace elements by ICP-MS.

Creator(s):

Kawamoto, Tatsuhiko; ORCID: 0000-0002-6989-874X
Taniuchi, Hajime; ORCID: 0000-0003-1147-4538
Kurihara, Keisuke
Hihara, Aya
Tasaka, Miki; ORCID: 0000-0002-5214-9849
Matsumoto, Akiko; ORCID: 0000-0002-4097-1763
Kuritani, Takeshi; ORCID: 0000-0002-0254-9115

Abstract:

Whole-rock composition of the spinel peridotite, plagioclase lherzolite, and mafic rocks from the Horoman peridotite complex, Japan. Major elements and Sc, V, Cr, Co, and Ni were measured by XRF, and the other trace elements by ICP-MS in EarthChem-bulk_rock_composition_data Horoman (excel file). EarthChem-Major_elements_minerals_with_EPMA (excel file).

How to cite this dataset:

Kawamoto, T., Taniuchi, H., Kurihara, K., Hihara, A., Tasaka, M., Matsumoto, A., Kuritani, T., 2026. Whole-rock major and trace element compositions of peridotite and mafic rock samples from the Horoman Peridotite Complex, Japan. Major elements and Sc, V, Cr, Co, and Ni were measured by XRF and the other trace elements by ICP-MS., Version 1.0. Interdisciplinary Earth Data Alliance (IEDA). https://doi.org/10.60520/IEDA/114440. Accessed 2026-04-13.

DOI Creation Date:

2026-04-06

License:

Creative Commons Attribution 4.0 International [CC-BY-4.0]

Keyword(s):

Coverage Scope: Regional (Continents, Oceans)
Geographic Location: Orogenic peridotite massif, mid-oceanic ridge, Horoman, Japan

User Contributed Keyword(s):

melt infiltration, olivine accumulation, mantle refertilization, Ti-zoning, Horoman peridotite

Data Available On:

2026-04-08

Resource Type:

Dataset

Dataset Information

DOI: 10.60520/IEDA/114440

Whole-rock major and trace element compositions of peridotite and mafic rock samples from the Horoman Peridotite Complex, Japan. Major elements and Sc, V, Cr, Co, and Ni were measured by XRF and the other trace elements by ICP-MS.