The continental crust in the overriding plate of the India-Asia collision zone in southern Tibet
is characterized by an overthickened layer of felsic composition with an underlying granulite …

The thin-skin Sevier and thick-skin Laramide belts of the North American Cordillera provide
a long-term record of the interrelations between evolving styles of mountain building and …

The Himalayan-Tibetan orogen culminated during the Cenozoic India--Asia collision, but its
geological framework and initial growth were fundamentally the result of multiple, previous …

Although widely used, classification schemes for granitic rocks have until now failed to
separate slab failure from arc magmatism in collisional orogens. Our previous work showed …

The Treatise on Geochemistry is the first work providing a comprehensive, integrated
summary of the present state of geochemistry. It deals with all the major subjects in the field …