Guillaume Duclaux
The usual place Room 2G16c, 2nd floor, Realfabyyget, 41 Allégaten, Bergen, NorwayThree-dimensional thermo-mechanical modelling unravels the complex deformation history of oblique rifts, transtensional margins, and gneiss domes Throughout the Wilson cycle the obliquity between lithospheric plate motion direction and nascent or existing plate boundaries prompts the development of intricate three-dimensional (3-D) …