Convergent plate motion at∼ 320–210 Ma generated the Tongbai-Dabie-Sulu (east-central
China)-Imjingang-Gyeonggi (central Korea)-Renge-Suo (Southwestern Japan)-Sikhote-Alin …

The tectonic evolution of the circum-Arctic, including the northern Pacific, Siberian and North
American margins, since the Jurassic has been punctuated by the opening and closing of …

Many aspects of deep-time Earth System models, including mantle convection,
paleoclimatology, paleobiogeography and the deep Earth carbon cycle, require high …

Palaeozoic to early Mesozoic terranes of the North American Cordillera mostly originated
from three distinct regions in Palaeozoic time: the western peri-Laurentian margin, western …

Abstract The Red Chris porphyry Cu-Au deposit is located in the Stikinia island-arc terrane
in northwest British Columbia. It is hosted by the Red Stock, which has five phases of …

Convergent plate boundaries are characterized by the development of crustal orogenic
wedges and orogenic plateaus but also by gravitational collapse of previously thickened …

Plate reconstructions since the breakup of Pangaea are mostly based on the preserved
spreading history of ocean basins, within absolute reference frames that are constrained by …

Crustal blocks accreted to North America form two major belts that are separated by a tract of
collapsed Jurassic–Cretaceous basins extending from Alaska to Mexico. Evidence of …

Abstract The allochthonous, pericratonic Yukon-Tanana terrane (YTT) underlies much of
southwest Yukon, easternmost Alaska and the Coast and Cassiar mountains of northern BC …

Paired belts of alkalic and calc-alkalic porphyry deposits are genetically linked to early
Mesozoic volcanic arcs preserved as the Quesnel and Stikine terranes in western Canada …