Rifted margins are regions at the transition from oceanic to continental crust, formed by the stretching and thinning of the Earth’s lithosphere before the creation of new ocean basins. The study focused on three key transects across Atlantic rifted margins. In their 2013 article in Marine and Petroleum Geology, Peron-Pinvidic et al. present a comparative analysis of the architecture of vari ...[Read More]
TS Must-Read – Peron-Pinvidic et al. (2013) Structural comparison of archetypal Atlantic rifted margins: A review of observations and concepts
.jpg){kind=link}