Megaestructuras online dating
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Continental growth in a margin setting can proceed by accretionary offscraping of juvenile material from the oceanic plate and by magmatic additions, whereas net mass loss can be achieved by subducting continental material, delamination, and chemical weathering.
In southcentral Chile, margin evolution was never interrupted by island-arc accretion or continental collision.
Thus, the area provides an excellent field laboratory for studying mass flux through a long-term, persistent, convergent-margin system.
Using new isotopic age data, we summarize the current knowledge of the geological evolution of the south-central Chilean margin, from subduction initiation to the ongoing Andean morphotectonic processes, with emphasis on mechanisms of mass transfer.
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