Gang Lu
Kontinentalsokkelen (2G16e) Realfagbygget, Allégaten 41, Bergen, NorwayRifting models with magmatism
Rifting models with magmatism
Seismic Waveform Modelling
Seismic Modelling of Normal Faults
Hot rocks under our feet; seismic reflection imaging of the processes and products of crustal magmatism Volcanoes are hot, loud and scary, thus we know little of their internal structure or underlying 'plumbing systems'. Magma intrusion in the Earth's crust, and …
Underneath the volcano: Trying to understand how igneous sills are emplaced using outcrops and seismic from East Greenland Here I will tell you about our ongoing work to understand sill emplacement, using data from Jameson Land in East Greenland. …
More details soon !
Relative continent/mid-ocean ridge elevation: a reference case for isostasy in geodynamics The choice on crustal and mantle densities in numerical geodynamics model is usually based on common habits. However, lithospheric deformation involving regional or fault-related flexure or involving strong change …
Salt Tectonics in the Santos Basin, Brazil: the effects of translation, base-salt relief and the enigma of the Albian Gap Salt-driven translation over variable base‐salt relief produces three‐dimensionally complex and multiphase deformation. Understanding how pre- and base-salt structures influence salt‐related …
Evolution of rift structures, topography and the sediment supply – A perspective from numerical modelling on the respective importance of tectonic and earth surface processes during continental rifting Lorenz Michel Continental rifting is the response of the continental lithosphere to …