The Trans-Mexican Volcanic Belt (TMVB) is a 1000km long Neogene continental arc
showing a large variation in composition and volcanic style, and an intra-arc extensional …

An extensive compilation of crustal thicknesses is used to develop crustal models in
continental South America. We consider point crustal thicknesses from seismic refraction …

We present a revised model for the opening of the South Atlantic Ocean founded on a
remapping of the continent—ocean boundaries and Aptian salt basins, the chronology of …

Presenting a coherent synthesis of lithosphere studies, this book covers a range of
geophysical methods (seismic reflection, refraction, and receiver function methods; elastic …

We present an upgraded version of a previously published 3-D density model of the Andean
subduction zone between 18° S and 45° S. This model consists of 3-D bodies of constant …

Diverse techniques have been applied over the past decade to quantify the uplift history of
the central Andean Plateau (AP). In this study, opposing models for surface uplift are …

How flat slab geometries are generated has been long debated. It has been suggested that
trenchward motion of thick cratons in some areas of South America and Cenozoic North …

Detailed information on lateral variations in lithospheric properties can aid in understanding
how surface deformation relates to deep Earth processes. The effective elastic thickness, Te …

Several lines of evidence have previously been used to suggest that ice retreat after the last
glacial maximum (LGM) resulted in regionally-increased levels of volcanic activity. It has …

Here, we examine spatiotemporal variations of Jurassic–Cretaceous magmatism along a c.
1000‐km transect across eastern Asia, including SW J apan, the Korean, J iaodong and …