The Szamotuly Graben covers the southernmost part of Permo-Mesozoic Poznan–Szamotuly Fault Zone. Along this regional discontinuity there are several salt structures, including diapir, over which an extensional graben formed in Paleogene and Neogene. is located north Poznan central-western Poland, NW–SE-trending, ~20 km long, 3–5.5 wide, up to 160 m deep. It filled with Lower Oligocene Neogene s...

The Vardar Zone is a product of the Triassic-Jurassic opening Neotethys, Jurassic obduction, Late Cretaceous/Paleogene consumption oceanic crust and continental collision. During last process, Eastern was thrust over Central eventually both onto Western Zone. present paleomagnetic structural study provided new results from first two zones in Belgrade area. younger set data, together with publis...

Abstract The Cenozoic history of the Tibetan Plateau topography is critical for understanding evolution Indian‐Eurasian collision, climate, and biodiversity. However, long‐term growth landscape remain ambiguous, it remains unclear if plateau uplift occurred soon after India‐Asia collision in Paleogene (∼50–25 Ma) or later Neogene (∼20–5 Ma). Here, we reproduce southeastern using a 2D model, whi...