New paleomagnetic data indicate that northwestern Costa Rica was located within 10 degrees from the equator throughout the Cretaceous (1)
The western Caribbean subduction zone initiated in Late Cretaceous time, in an intraoceanic setting, breaking up lithosphere of at least 70 Myr old (1)
We reconstructed the Jurassic-Cretaceous plate tectonic history of the Caribbean Plate within the Mesozoic Panthalassa Ocean (1)