Is Fe-Ti type orogenic peridotite of crustal cumulate origin? Implication from Svartberget garnet peridotite/pyroxenite (Western Gneiss Complex, SW Norway)

Graph neighborhood for 'Is Fe-Ti type orogenic peridotite of crustal cumulate origin? Implication from Svartberget garnet peridotite/pyroxenite (Western Gneiss Complex, SW Norway)'. Click aggregate nodes to navigate.
ADS bibcode
2017AGUFM.V31B0507Y
year
2017
Listed Authors
Yui, T. F.
Chu, H. T.
Shen, P.
Hwang, S. L.
Cuthbert, S. J.
Listed Institutions
Academia Sinica, Taipei, Taiwan
Central Geological Survey, Taipei, Taiwan
Department of Materials and Optoelectronic Science, National Sun Yat-sen University, Kaohsiung, Taiwan
Department of Materials Science and Engineering, National Dong Hwa University, Hualien, Taiwan
Univ of the West of Scotland, Paisley, United Kingdom

Linked Authors [?]

Linked Institutions