Origin of chromite in mafic–ultramafic-hosted hydrothermal massive sulfides from the Main Uralian Fault, South Urals, Russia

S.G Tesalina, P Nimis, T Augé, V.V Zaykov

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DOI: 10.1016/s0024-4937(03)00090-2
Published: 2003-09
Container: Lithos
Publisher: Elsevier BV
Open access: unknown

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Cite this work

BibTeX

@article{allodium:10.1016/s0024-4937-03-00090-2,
  title = {Origin of chromite in mafic–ultramafic-hosted hydrothermal massive sulfides from the Main Uralian Fault, South Urals, Russia},
  author = {S.G Tesalina and P Nimis and T Augé and V.V Zaykov},
  year = {2003},
  journal = {Lithos},
  doi = {10.1016/s0024-4937(03)00090-2},
  url = {https://doi.org/10.1016/s0024-4937(03)00090-2}
}

RIS

TY  - JOUR
TI  - Origin of chromite in mafic–ultramafic-hosted hydrothermal massive sulfides from the Main Uralian Fault, South Urals, Russia
AU  - S.G Tesalina
AU  - P Nimis
AU  - T Augé
AU  - V.V Zaykov
PY  - 2003
JO  - Lithos
DO  - 10.1016/s0024-4937(03)00090-2
UR  - https://doi.org/10.1016/s0024-4937(03)00090-2
ER  -

APA

Tesalina, S., Nimis, P., Augé, T., & Zaykov, V. (2003). Origin of chromite in mafic–ultramafic-hosted hydrothermal massive sulfides from the Main Uralian Fault, South Urals, Russia. Lithos. https://doi.org/10.1016/s0024-4937(03)00090-2

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crossref · retrieved 2026-09-26T08:54:47.096Z