Articles tagged with Tectonic Plates
Researchers at UC Davis and MIT propose a new model of Earth's mantle as two layers, reconciling conflicting evidence from seismologists and geochemists. The new model suggests that tectonic plates encounter a geological barrier in the lower mantle, preventing them from mixing with deep-mantle material.
The Cornell team will monitor seismic waves produced by local and distant earthquakes using temporary recording stations set up in eastern Turkey. They aim to determine how the Arabian plate is being supported and what specific earthquake hazards exist in the region, shedding light on the early stages of continental collision.
Researchers have discovered motion along the southern portion of the boundary between the west African (Nubian) and east African (Somalian) plates. The finding helps geologists understand how the East African rift fits into plate tectonics, improving global models for predicting India-Eurasia collision.
Scientists discover African Superswell is caused by hot mantle material rising from the core-mantle boundary, elevating southern Africa and driving tectonic plates. This phenomenon, known as dynamic topography, reveals a link between deep mantle dynamics and surface features.
The Global Positioning System (GPS) is enabling geologists to study earthquakes in real time, revealing incremental motion and slow squeezing within plates that can lead to earthquakes. This technology is improving earthquake hazard studies by allowing for more accurate predictions of seismic activity.
Researchers use GPS satellites to monitor the movement of an entire continent and record the yearly growth of the Andes Mountains. The study shows that satellite data can help geologists calculate accumulating stresses along fault lines, promising improved earthquake hazard estimation.
Researchers discover the San Andreas fault cuts straight through the crust and Moho, affecting stress buildup and earthquake hazard predictions. The study improves understanding of rock boundaries, types, and stress accumulation to better assess seismic risks.
Researchers found calcite grains in mid-continent areas showed deformation patterns consistent with shearing stress, contradicting the idea that these regions are 'quiet and tectonically dead'. The study provides new insights into tectonic processes and offers critical input for computer modeling of plate dynamics.
A revised ocean depth model developed by Northwestern University geologists significantly better fits observed data, correcting inconsistencies in existing models. By adjusting the assumed thickness of the lithosphere to 95 kilometers, the new model accurately predicts ocean depths surrounding the Hawaiian Islands.
A team of scientists has assembled evidence on rocks and rock formations deep beneath the surface to locate an ancient strike-slip fault. If successful, this will provide opportunities to study geological processes in the lower crust during strike-slip faulting.
A recent earthquake in Peru has bolstered a researcher's theory that large earthquakes will not occur in a specific region near the quake site. The study found a correlation between plate shape and seismic activity, identifying areas of low seismicity called seismic gaps.
Researchers will use Logging While Drilling technology to sample physical and chemical properties of rocks and sediments on the ocean floor. They aim to determine the age, composition, and physical properties of the area's rocks and sediments, as well as understand why some areas have low heat flow.
A new model developed by University of California geophysicists predicts the size and shape of tectonic plates by assuming a 30-fold increase in mantle viscosity with depth. This assumption creates a cyclic flow or convection cell with dimensions close to the plate sizes, explaining why continents are broken into large plates.
Scientists at UC Berkeley developed a 3D model that explains the size and shape of tectonic plates, predicting they are larger than previously thought due to increased mantle viscosity. The model simulates convection cells in the mantle, resulting in large plates and subduction zones.