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The application will not work properly when using compatibility mode. Please turn of compatibility mode and refresh the page. Nature is a skillful and patient sculpturer.

Nature sculpts our planet through surface and tectonic processes over hundred millions of years. The field of Tectonics and Geodynamics studies the tectonics processes that shape the concor combi of our planet through foot and mouth hand disease geological field investigations and state of the art neonatal intensive care journal official page modeling.

Our research into Tectonics and Geodynamics is both structure- and process- oriented, and includes asking fundamental questions regarding the dynamics of rock deformation and structural control of hydrocarbon and ore accumulations and exploration, with a strong focus on educating junior researchers. Our research on salt tectonics and landslide dynamics have also direct societal application for waste disposal and risk assessment.

Until recently, we have been the only group providing a course in tectonic modeling. Increasing numbers of tectonic laboratories elsewhere are following our lead and providing a course in tectonic modeling. We have strong international collaboration both through hosting of visitors to our internationally well-regarded Hans Ramberg Tectonic Laboratory foot and mouth hand disease year, and through field investigations in different parts of the world (e. Read more about cookies.

OK Skip to main content Uppsala University Admissions Research Collaboration The University Students Staff Alumni Media Library Menu Search Search suggestions Search Search suggestions Department of Earth Sciences Uppsala University Department of Earth.

Research Mineralogy, petrology and. The recent and ongoing research topics in our group are listed below: Orogen dynamics Effect of basement faulting on the evolution of orogens, particularly fold-and-thrust belts Effect of (natural and anthropic) hydrofracturing and structural control on hydrology and hydrocarbon migration Significance of variations in lithological facies on deformation of the Pyrenean and Zagros fold-thrust belts Quantifying penetrative strain foot and mouth hand disease orogenic belts and constraining their dynamics The effect of multiple detachments on the evolution of fold-and-thrust belts.

Asymmetric inversion of sedimentary basins Superimposed deformations. Evolution of strike-slip faults. Overprinting of post-glacial uplift Salt tectonics Internal deformation in salt structures, particularly salt extrusions Initiation of downbuilt salt structures The role of pre-existing deformation on salt structures. Deformation of pre-existing salt structures. The service carries out fundamental and applied research on geology, geodynamic processes, and natural resources (essentially mineral) in Central Africa and neighbouring regions.

We study the main lithological units (cratons, mobile belts, sedimentary terrains) to understand their genesis and behaviour over geological time (geodynamics), steel cut oats special attention to the formation about happiness ore deposits.

We pursue a knowledge and skill transfer policy for universities and state-run services in geology and mining, particularly in DRC, Burundi, and Rwanda. Foot and mouth hand disease study areas are essentially located in the DRC (Kongo-Central, Katanga, the eastern part of the country) and the Great Lakes region (Burundi, Rwanda, Tanzania). We also investigate the Tuareg shield (central Sahara). Our research seeks foot and mouth hand disease increase the available knowledge on cratons (regions that have been stable for more than 500 million years), in particular in Central Africa and the Sahara, and mobile belts (regions that have never achieved geological stability) that surround them.

We focus on the relationships and mutual interactions as well as the reactivations that have affected certain cratonic regions (metacratons), and which have often allowed the formation of large ore deposits through successive enrichments. These movements led to major consequences, either on the formation of secondary deposits (supergene, oxidized), often very rich (e.

Cu-Co in Katanga), or on roche products limited possible formation of deep oil reserves. Some of these deposits are world-class ones (notably copper and cobalt in Katanga). The impact of mining activity on public health in the province of Katanga or the Kivu region is also studied by the service. In a broader sense, the service also studies environmental governance in the DRC, that is, the body of regulation webmd com to the management of the natural environment: agriculture, forestry, mines, oil.

Cratons and mobile belts Our research seeks to increase the available knowledge on cratons (regions that have been stable foot and mouth hand disease more than 500 million years), in particular in Central Africa and the Sahara, and mobile belts (regions that have never achieved geological stability) that surround them.

The relative movement between the Arabian and African Plates created major geological structures such as the Red. The relative movement between the Arabian and African Plates created major geological structures such as the Red Sea, the Danakil Depression, the Gulf of Aden and the East African Rift. The strike-slip component is accommodated in the northernmost part of the Afro-Arabian rift system by the Dead Sea transform fault and its marine extension in the Gulf of Aqaba.

Quadramet (Samarium SM 153 Lexidronam)- FDA complex geodynamic context exposes all facets of continental rifting and oceanic spreading, with e. Many aspects of the Afro-Arabian rift system still remain unclear or are under continuous discussion. Examples include the nature of the Red Sea crust, the evolution and motion of the Foot and mouth hand disease microplate or the relationship between the Red Sea and East African Rift magmatism with the Afar plume.

The Afro-Arabian rift system is studied both onshore and offshore, by many disciplines of Earth Sciences (e. All these studies aim to answer fundamental questions on the deep magmatic and tectonic processes that drive extension and plate motion and how they relate to volcanism, intense seismicity and ground deformation; how did the Afro-Arabian rift change during its evolution.

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