Mineralogy, composition and PGM of chromitites from Pefki, Pindos ophiolite complex (NW Greece): evidence for progressively elevated fAs conditions in the upper mantle sequence

Research output: Contribution to journalArticleResearchpeer-review

Standard

Mineralogy, composition and PGM of chromitites from Pefki, Pindos ophiolite complex (NW Greece): evidence for progressively elevated fAs conditions in the upper mantle sequence. / Kapsiotis, A.; Grammatikopoulos, Tassos; Tsikouras, B. et al.
In: Mineralogy and Petrology, 2011, p. 129-150.

Research output: Contribution to journalArticleResearchpeer-review

Bibtex - Download

@article{8c7a2e470a61472d8f58862891a90e19,
title = "Mineralogy, composition and PGM of chromitites from Pefki, Pindos ophiolite complex (NW Greece): evidence for progressively elevated fAs conditions in the upper mantle sequence",
author = "A. Kapsiotis and Tassos Grammatikopoulos and B. Tsikouras and K. Hatzipanagiotou and Federica Zaccarini and Giorgio Garuti",
year = "2011",
language = "English",
pages = "129--150",
journal = "Mineralogy and Petrology",
issn = "0930-0708",
publisher = "Springer Wien",

}

RIS (suitable for import to EndNote) - Download

TY - JOUR

T1 - Mineralogy, composition and PGM of chromitites from Pefki, Pindos ophiolite complex (NW Greece): evidence for progressively elevated fAs conditions in the upper mantle sequence

AU - Kapsiotis, A.

AU - Grammatikopoulos, Tassos

AU - Tsikouras, B.

AU - Hatzipanagiotou, K.

AU - Zaccarini, Federica

AU - Garuti, Giorgio

PY - 2011

Y1 - 2011

M3 - Article

SP - 129

EP - 150

JO - Mineralogy and Petrology

JF - Mineralogy and Petrology

SN - 0930-0708

ER -