Using combined seismic refraction/wide-angle reflection method project Alp 2002 explored the contact zone between South-Eastern Alps, Dinarides and Pannonian basin.
Andrej Gosar
doaj
Mantle Transition Zone Thickness Beneath the Middle East: Evidence for Segmented Tethyan Slabs, Delaminated Lithosphere, and Lower Mantle Upwelling [PDF]
Ayoub Kaviani +5 more
openalex +1 more source
EarthScope applies modern observational, analytical, and telecommunications technologies to investigate the structure and evolution of the North American continent and the physical processes controlling earthquakes and volcanic eruptions.
Michelle Hall-Wallace
core +1 more source
Plume‐orogenic lithosphere interaction recorded in the Haladala layered intrusion in the Southwest Tianshan Orogen, NW China [PDF]
Peng‐Li He +5 more
openalex +1 more source
Supplemental Material: Permian plume-strengthened Tarim lithosphere controls the Cenozoic deformation pattern of the Himalayan-Tibetan orogen [PDF]
Xu Xi, Hanlin Chen, et al.
openalex +1 more source
Tectonic evolution of a continental collision zone: A thermomechanical numerical model [PDF]
We model evolution of a continent-continent collision and draw some parallels with the tectonic evolution of the Himalaya. We use a large-scale visco-plasto-elastic thermomechanical model that has a free upper surface, accounts for erosion and deposition
Avouac, J.-P., Burov, E., Toussaint, G.
core
Convective removal of lithosphere beneath mountain belts; thermal and mechanical consequences [PDF]
J. P. Platt, Philip England
openalex +1 more source
Layered Mantle Lithosphere in the Lac de Gras Area, Slave Craton: Composition, Structure and Origin [PDF]
William L. Griffin +8 more
openalex +1 more source
The break-up of continents and the formation of new ocean basins
Rifted continental margins are the product of stretching, thinning and ultimate break-up of a continental plate into smaller fragments, and the rocks lying beneath them store a record of this rifting process.
Minshull, T.A.
core +1 more source

