PGE- and Os-isotope data of chromitites in the Shebeniku ophiolitic complex, Albania: evidence for two stage melting in a supra subduction zone environment

Henning Kocks; Thomas Meisel; Frank Melcher; K.-P. Burgath

PGE- and Os-isotope data of chromitites in the Shebeniku ophiolitic complex, Albania: evidence for two stage melting in a supra subduction zone environment

Henning Kocks
, Thomas Meisel
, Frank Melcher
, K.-P. Burgath

Chair of General and Analytical Chemistry (120)

Research output: Chapter in Book/Report/Conference proceeding › Conference contribution

Translated title of the contribution	PGE- and Os-isotope data of chromitites in the Shebeniku ophiolitic complex, Albania: evidence for two stage melting in a supra subduction zone environment
Original language	English
Title of host publication	PGE- and Os-isotope data of chromitites in the Shebeniku ophiolitic complex, Albania: evidence for two stage melting in a supra subduction zone environment
Publisher	EGU
Pages	508-508
Publication status	Published - 2006

Cite this

Kocks, H., Meisel, T., Melcher, F., & Burgath, K.-P. (2006). PGE- and Os-isotope data of chromitites in the Shebeniku ophiolitic complex, Albania: evidence for two stage melting in a supra subduction zone environment. In PGE- and Os-isotope data of chromitites in the Shebeniku ophiolitic complex, Albania: evidence for two stage melting in a supra subduction zone environment (pp. 508-508). EGU.

Kocks, Henning ; Meisel, Thomas ; Melcher, Frank et al. / PGE- and Os-isotope data of chromitites in the Shebeniku ophiolitic complex, Albania: evidence for two stage melting in a supra subduction zone environment. PGE- and Os-isotope data of chromitites in the Shebeniku ophiolitic complex, Albania: evidence for two stage melting in a supra subduction zone environment. EGU, 2006. pp. 508-508

@inproceedings{c4f31313fed74f03ac478b8390fb3bde,

title = "PGE- and Os-isotope data of chromitites in the Shebeniku ophiolitic complex, Albania: evidence for two stage melting in a supra subduction zone environment",

author = "Henning Kocks and Thomas Meisel and Frank Melcher and K.-P. Burgath",

year = "2006",

language = "English",

pages = "508--508",

booktitle = "PGE- and Os-isotope data of chromitites in the Shebeniku ophiolitic complex, Albania: evidence for two stage melting in a supra subduction zone environment",

publisher = "EGU",

}

Kocks, H, Meisel, T , Melcher, F & Burgath, K-P 2006, PGE- and Os-isotope data of chromitites in the Shebeniku ophiolitic complex, Albania: evidence for two stage melting in a supra subduction zone environment. in PGE- and Os-isotope data of chromitites in the Shebeniku ophiolitic complex, Albania: evidence for two stage melting in a supra subduction zone environment. EGU, pp. 508-508.

PGE- and Os-isotope data of chromitites in the Shebeniku ophiolitic complex, Albania: evidence for two stage melting in a supra subduction zone environment. / Kocks, Henning; Meisel, Thomas ; Melcher, Frank et al.
PGE- and Os-isotope data of chromitites in the Shebeniku ophiolitic complex, Albania: evidence for two stage melting in a supra subduction zone environment. EGU, 2006. p. 508-508.

Research output: Chapter in Book/Report/Conference proceeding › Conference contribution

TY - GEN

T1 - PGE- and Os-isotope data of chromitites in the Shebeniku ophiolitic complex, Albania: evidence for two stage melting in a supra subduction zone environment

AU - Kocks, Henning

AU - Meisel, Thomas

AU - Melcher, Frank

AU - Burgath, K.-P.

PY - 2006

Y1 - 2006

M3 - Conference contribution

SP - 508

EP - 508

BT - PGE- and Os-isotope data of chromitites in the Shebeniku ophiolitic complex, Albania: evidence for two stage melting in a supra subduction zone environment

PB - EGU

ER -

Kocks H, Meisel T , Melcher F, Burgath KP. PGE- and Os-isotope data of chromitites in the Shebeniku ophiolitic complex, Albania: evidence for two stage melting in a supra subduction zone environment. In PGE- and Os-isotope data of chromitites in the Shebeniku ophiolitic complex, Albania: evidence for two stage melting in a supra subduction zone environment. EGU. 2006. p. 508-508