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 – Brun (1999): Narrow rifts versus wide rifts: inferences for the mechanics of rifting from laboratory experiments
In 1999 Jean-Pierre Brun published his Must-Read paper about rifting, in which he reviews fifteen years of laboratory experiments at Geosciences Rennes. In a brief introduction the paper reminds the reader of the two main rift types: narrow rifting as the preceding stage for continental break-up, and wide rifting that occurs after cessation of convergence. The article introduces some key differenc ...[Read More]