John Longhi

Massif-type anorthosites and related granitoids result from post-collisional remelting of a continental arc root: the Sveconorwegian case

Polybaric fractionation and the connection between high-Al gabbro and monzonorite

Influence of the Sveconorwegian granulite metamorphism on the composition of the sources of the Sveconorwegian massif type anorthosites (Rogaland complex) and related granitoids

Sveconorwegian Massif Type Anorthosites (Rogaland Complex) and Penecontemporaneous Granitoids Suites Result From Postcollisional Remelting of Subduction-Related Underplated Mafic Cumulates

Phase diagram constraints on magma mixing in “underplated” magma chambers

Trace elements composition of massif type anorthosites's parent magma; constraints from experimental data on DSr (pag/melt) and DCr (opx/melt)

The charnockitic liquid line of descent of jotunites: constraints from experimental and petrological data

Experimental and geochemical constraints on the liquid line of descent of jotunites (hypersthene monzodiorites); implications for anorthosite petrogenesis

The effect of pressure on the partitioning of Sr between plagioclase and melt and Cr between orthopyroxene and melt: implications for anorthosite genesis

A mantle-derived parent massif anorthosites