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 …

Continental arcs in Cordilleran orogenic systems display episodic changes in magma
production rate, alternating between flare ups (70–90 km 3 km− 1 Myr− 1) and lulls (< 20 km …

位于青藏高原南部的冈底斯岩浆弧是新特提斯大洋岩石圈长期俯冲导致的中生代岩浆作用的
产物, 而且在印度与亚洲大陆碰撞过程中叠加了强烈的新生代岩浆作用, 是世界上典型的复合型 …

Reconfigurations of magmatic arcs through time have been recognized since pioneering
works, describing inland and trenchward arc migrations or magmatic shut-off lasting for …

Abstract Upper Cretaceous–Eocene forearc strata deposited along the California continental
margin record a complex history of plate convergence that shaped the tectonic development …

Arclogites are eclogite-like rocks formed magmatically as ultramafic residues and cumulates
in the roots of thick arcs (Ducea et al., 2021 companion paper). They are inferred to be …

This Chapter considers triple oxygen isotope variations and their 4 Gyr temporal evolution in
bulk siliciclastic sedimentary rocks and in granites. The d18O and∆′ 17O values provide …

Magmatic activity in continental arcs is known to vary in a non-steady-state manner, with the
mechanisms driving magmatic activity being a matter of ongoing discussion. Of particular …

We investigate the temporal record of magmatism in the Fiordland sector of the Median
Batholith (New Zealand) with the goal of evaluating models for cyclic and episodic patterns …

In this study, structures in plutons and host rocks are coupled with geochronology to track
paleodeformation fields from the late Paleozoic to Late Cretaceous in the central Sierra …