Deciphering the magmatic history of continental magmatic arcs, in general, and the growth
history of individual intrusions, in particular, is key to understanding the complex history of …

Isochemical pressure–temperature phase-diagram sections portray the theoretical
equilibrium distribution of mineral assemblages and mineral compositions for a given bulk …

Chemically zoned garnets provide a record of the changing conditions within the tectonically
evolving crust where metamorphic mineral growth occurs. Recent advances in Sm–Nd …

Abstract The Oaxacan Complex represents the largest outcrop of late Mesoproterozoic age,
granulite-facies metamorphic rocks in Mexico. The southwestern Oaxacan Complex was …

Pembroke Granulite from Fiordland, New Zealand provides a window into the mid-to lower
crust of magmatic arcs. Garnet Sm–Nd and zircon U–Pb ages constrain the timing and …

The growth of the Coast Mountains batholith has been documented as episodic through
time, and it has become a type example of a continental arc system that developed through …

PT pseudosections, constructed in MnNCKFMASH and adjusted for chemical compositional
changes resulting from zoned garnet growth (chemical fractionation) in a pelitic rock, show …

A quantitative assessment of metamorphic chemical equilibrium derived from correlation of
spessartine content and garnet Sm–Nd ages suggests that major element matrix equilibrium …

Garnet granulite facies mid‐to lower crust in Fiordland, New Zealand, provides evidence for
pulsed intrusion and deformation occurring in the mid‐to lower crust of magmatic arcs. 238U …

One of the key aims of geochronology, and the subject of the papers in this Special
Publication, is the linkage of isotopic ages to petrological and textural information. A close …