作者: S.F. Foley , G.M. Yaxley , A. Rosenthal , S. Buhre , E.S. Kiseeva
DOI: 10.1016/J.LITHOS.2009.03.020
关键词: Solidus 、 Metasomatism 、 Peridotite 、 Silicate 、 Kimberlite 、 Chemical composition 、 Partial melting 、 Geology 、 Ultramafic rock 、 Geochemistry
摘要: Partial melting experiments at 40, 50 and 60 kbar pressure on three peridotite compositions with 0.5–0.63 wt.% H 2 O and 2.0–3.2 wt.% CO 2 added indicate melting temperatures only …