The largest tectonic relief breaking the Earth's surface (13 km vertically) is at the subduction margin of the Andes, which generates routinely megathrust earthquakes (Mw> 8.5) and …
L Giambiagi, A Tassara, A Echaurren, J Julve… - Earth-Science …, 2022 - Elsevier
As the archetype of mountain building in subduction zones, the Central Andes has constituted an excellent example for investigating mountain-building processes for decades …
Current end-member models for the geodynamic evolution of orogenic plateaus predict (a) slow and steady rise during crustal shortening and ablative subduction (ie, continuous …
JB Barnes, TA Ehlers - Earth-Science Reviews, 2009 - Elsevier
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 …
Magnetite-(apatite) ore deposits are interpreted as being formed by the crystallization of iron- rich ultrabasic melts, dominantly generated by the interaction of silicate melts with oxidized …
The origins of Kiruna-type magnetite (-apatite)[Mt (-Ap)] deposits are contentious, with existing models ranging from purely hydrothermal to orthomagmatic end members. Here, we …
Mountainous areas host a disproportionately large fraction of Earth's biodiversity, suggesting a causal relationship between mountain building and biological diversification. Mountain …
F Tornos, F Velasco, JM Hanchar - Economic Geology, 2017 - pubs.geoscienceworld.org
The geology and geochemistry of the El Laco iron oxide deposit (Central Andes, Chile) support a genesis related to the ascent, degassing, and subvolcanic emplacement of an …
Quantifying interactions between uplift, climate, deformation, and exhumation remains difficult, in many cases due to a paucity of data relevant to all processes. We synthesize new …