This dissertation investigates the evolution of continental orogenic systems in Central Asia during and between pre-collisional plate convergence (Cordilleran-style orogenesis), syn-collisional plate convergence (collisional orogenesis), and post-collisional tectonic processes within the scope of closing Paleo-Asian and Tethyan ocean basins. A brief introductory chapter outlines the scope and context of the research. Appendix A focuses on the Late Paleozoic closure of the Turkestan ocean basin and subsequent collision between the Karakum–Tarim and Kazakh–Kyrgyz terranes in the South Tian Shan, within the scope of the final amalgamation of the Mesoproterozoic–Permian Central Asian Orogenic Belt. Appendix B focuses on late Cenozoic syn-collis...
The Central Asian Orogenic Belt (CAOB) evolved through complex closure of the Paleo-Asian Ocean from...
This journal issue entitled: Geodynamic evolution of Central Asia in the Paleozoic and MesozoicThe A...
International audienceThe Central Asian Orogenic Belt (CAOB) represents one of the largest Phanerozo...
International audienceDuring the Late Palaeozoic–Mesozoic, Central Asia and Tibet were affected by s...
This paper reviews and integrates new results on: (I) the Late Paleozoic and Mesozoic evolution of C...
International audienceThe tectonic evolution of the Central Asian Orogenic Belt (CAOB) is characteri...
The Paleozoic mosaic-block structure of the Central Asia folded area is formed by isometrically outl...
In the end of the 20th century folded structures of central Asia were regarded as formed by accretio...
This dissertation research addresses the tectonism of continental crust during ocean basin closure, ...
The Central Asian foldbelt has been regarded to be a result of accretion-collisional processes event...
The Central Asian Orogenic Belt (CAOB) is one of the world's largest accretionary orogens, which was...
International audienceThe Altaid tectonic collage extends over Central Asia, exposing numerous accre...
The Altaids, one of the largest and long-lived accretionary orogens in the world, developed from ca....
The Central Asian Orogenic Belt (CAOB) was the result of long-lived multi-stage tectonic evolution, ...
The Central Asian Orogenic Belt (CAOB) evolved through complex closure of the Paleo-Asian Ocean from...
This journal issue entitled: Geodynamic evolution of Central Asia in the Paleozoic and MesozoicThe A...
International audienceThe Central Asian Orogenic Belt (CAOB) represents one of the largest Phanerozo...
International audienceDuring the Late Palaeozoic–Mesozoic, Central Asia and Tibet were affected by s...
This paper reviews and integrates new results on: (I) the Late Paleozoic and Mesozoic evolution of C...
International audienceThe tectonic evolution of the Central Asian Orogenic Belt (CAOB) is characteri...
The Paleozoic mosaic-block structure of the Central Asia folded area is formed by isometrically outl...
In the end of the 20th century folded structures of central Asia were regarded as formed by accretio...
This dissertation research addresses the tectonism of continental crust during ocean basin closure, ...
The Central Asian foldbelt has been regarded to be a result of accretion-collisional processes event...
The Central Asian Orogenic Belt (CAOB) is one of the world's largest accretionary orogens, which was...
International audienceThe Altaid tectonic collage extends over Central Asia, exposing numerous accre...
The Altaids, one of the largest and long-lived accretionary orogens in the world, developed from ca....
The Central Asian Orogenic Belt (CAOB) was the result of long-lived multi-stage tectonic evolution, ...
The Central Asian Orogenic Belt (CAOB) evolved through complex closure of the Paleo-Asian Ocean from...
This journal issue entitled: Geodynamic evolution of Central Asia in the Paleozoic and MesozoicThe A...
International audienceThe Central Asian Orogenic Belt (CAOB) represents one of the largest Phanerozo...