FM Schneider, X Yuan, B Schurr… - Journal of …, 2019 - Wiley Online Library
Abstract The Cenozoic convergence between India and Asia has created Earth's thickest crust in the Pamir‐Tibet Plateau by extreme crustal shortening. Here we study the crustal …
Abstract The Acadian and Neoacadian orogenies are widely recognized, yet poorly understood, tectono-thermal events in the New England Appalachian Mountains (USA). We …
Different crustal deformation histories between Tibet and the Pamir reflect along‐strike variations in geodynamics of the Tethys orogen. To investigate the less well‐documented …
Rare earth element (REE) signatures of high‐U/Pb and high‐Th/Pb accessory minerals are typically used to link their ages to specific petrological processes ('petrochronology')—most …
Several extrusion mechanisms have been proposed to explain the occurrences of ultra-high pressure (UHP) rocks at collisional margins. Here we assess the suitability of the channel …
Neogene, syn‐collisional extensional exhumation of Asian lower–middle crust produced the Shakhdara–Alichur gneiss‐dome complex in the South Pamir. The< 1 km‐thick, mylonitic …
Despite Miocene extension and exhumation of middle to lower crust in a series of gneiss domes and interpreted Cenozoic delamination of the lower crust, the crust in the modern …
Seismologic and geologic fault‐slip data characterize the active deformation of the intramontane Tajik basin and its margins, the Tian Shan, Pamir, and Hindu Kush at the …
MA Smit, JC Vrijmoed, EE Scherer… - Journal of …, 2024 - Wiley Online Library
Incorporation of rare earth elements (REE) in garnet enables garnet chronology (Sm‐Nd, Lu‐ Hf), and imparts a garnet‐stable signature on cogenetic phases, which allows …