Appinite–granite suites commonly occur in the final stage of collisional orogenic processes,
providing a unique opportunity to reveal the properties of continental lithospheric mantle and …

Appinite rock suites generally consist of bimodal mafic–silicic hornblende-bearing igneous
rocks, mostly generated by post-subduction processes along ancient convergent plate …

The Johnston Complex represents a rare inlier of the Neoproterozoic basement of southern
Britain and offers a window into the tectonomagmatic regime of East Avalonia during the …

ABSTRACT The Western Cordillera of Colombia preserves the remnants of the Cretaceous
tectonic history of the northernmost Andes, including fragments of Ecuadorian-Colombian …

Abstract The Variscan Orogen was formed during the closure of the Rheic Ocean and the
final collision between the North American and West African cratons in the Late Paleozoic …

Granitic plutons dominated by felsic-intermediate compositions are commonly spatially and
temporally associated with mafic intrusions; however, the genetic relationship between the …

Special Publication 542 is a tribute to the remarkable career of J. Brendan Murphy and
features 32 articles by 134 authors from 17 different countries; a testament to the high-profile …

This volume is a tribute to the career of J. Brendan Murphy and features papers by over 100
authors from countries all over the world: a testament to the high-profile and far-reaching …

Appinite–granite suites commonly occur in the final stage of collisional orogenic processes,
providing a unique opportunity to reveal the properties of continental lithospheric mantle and …