Supercooled diopside melt: confirmation of temperature-dependent expansivity using container-based dilatometry Joachim GottsmannDonald B. Dingwell Pages: 127 - 135
Experimental study of the K2ZrSi3O9 (wadeite)–K2TiSi3O9 and K2(Zr,Ti)Si3O9–phlogopite systems at 2–3 GPa Andrea OrlandoYves ThibaultAlan D. Edgar Pages: 136 - 145
The compositional variation of synthetic sodic amphiboles at high and ultra-high pressures P. TropperC. E. ManningL.-S. Kao Pages: 146 - 162
Fluid inclusions as metamorphic process indicators in the Southern Aravalli Mountain Belt (India) Ronald J. BakkerManish A. Mamtani Pages: 163 - 179
Titaniferous magnetite–ilmenite thermometry and titaniferous magnetite–ilmenite–orthopyroxene–quartz oxygen barometry in granulite facies gneisses, Bamble Sector, SE Norway: implications for the role of high-grade CO2-rich fluids during granulite genesis Daniel E. Harlov Pages: 180 - 197
An Archean arc basalt–Nb-enriched basalt–adakite association: the 2.7 Ga Confederation assemblage of the Birch–Uchi greenstone belt, Superior Province P. HollingsR. Kerrich Pages: 208 - 226
Fingerprinting feldspar phenocrysts using crystal isotopic composition stratigraphy: implications for crystal transfer and magma mingling in S-type granites Tod E. WaightRoland MaasIan A. Nicholls Pages: 227 - 239
Comment on: “Enriched mantle – Dupal signature in the genesis of the Jurassic Ferrar tholeiites from Prince Albert Mountains (Victoria Land, Antarctica)” by Antonini P. et al. (Contributions to Mineralogy and Petrology 136, 1–19; 1999) Janet Hergt DISCUSSION Pages: 240 - 244
Reply to the comment by J. Hergt on the paper “Enriched mantle – Dupal signature in the genesis of the Jurassic Ferrar tholeiites from Prince Albert Mountains (Victoria Land, Antarctica)” by Antonini et al. (Contributions to Mineralogy and Petrology 136: 1–19, 1999) P. AntoniniE. M. PiccirilloG. Orsi REPLY Pages: 245 - 249
