We believe that many Mesozoic and Cenozoic obducted ophiolite belts of SE Asia are fragments of fore-arc or back-arc lithosphere. |
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Melts of these metasomites were volatile rich and hence ascended rapidly through the lithosphere, forming the lamprophyre magmas. |
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In plate tectonics, a transform fault is a strike-slip fault extending throughout the lithosphere and joining any two other plate margins. |
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After obduction, there was a slow rate of subsidence, which reflects the continuing cooling of the underlying Indian lithosphere after rifting. |
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As you pull the lithosphere apart, as it separates, decompression occurs in the earth's mantle underneath the spreading centre. |
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Slow and highly attenuating lithosphere exists beneath this portion of the Anatolian plate and geometry of the Benioff zones. |
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After new oceanic crust forms, the lithosphere cools and thickens as it moves away from the ocean ridge. |
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The differences between them arise as a result of the differences in strength and density of oceanic and continental lithosphere. |
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Scientists believe that below the lithosphere is a relatively narrow, mobile zone in the mantle called the asthenosphere. |
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This requires the removal of 80-100 km of Archaean lithosphere since Mesozoic time. |
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Across the ridge, the asymmetric flow pattern in the asthenosphere will cause differential drag at the base of the lithosphere. |
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It starts with the lithosphere, goes on to atmosphere and hydrosphere, and ends up with the biosphere. |
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An alternative to an active mantle thermal anomaly is greater stretching of the mantle lithosphere than the crust. |
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This allows us to place much tighter constraints on the tectonic and thermal evolution of the lithosphere during late orogenic extension than has previously been possible. |
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The near-constant depth of the abyssal sea floor indicates that the lithosphere thickens to roughly 100 km in 70 million years, but then ceases to grow. |
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Diamonds are most commonly associated with Archean subcontinental lithosphere but nanodiamonds were recently reported from mantle xenoliths in EM1like Hawaiian basalts. |
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For example, the discovery of hydrothermal vents in the 1970s offered a clear proof of significant dynamic connections between the lithosphere, hydrosphere and biosphere. |
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These igneous rocks record the extensive magmatism that resulted from northward subduction of Neotethyan oceanic lithosphere beneath the Lhasa terrane. |
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The lithosphere is the rigid outermost layer of the geosphere. |
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Because the radioactive source of heat is deep within the mantle, the fluid asthenosphere circulates as convection currents underneath the solid lithosphere. |
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The lithosphere is cooler and more rigid, while the asthenosphere is hotter and flows more easily. |
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Somehow, this energy must be transferred to the lithosphere for tectonic plates to move. |
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Bostrom presented evidence for a general westward drift of the Earth's lithosphere with respect to the mantle. |
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The foreland basin forms ahead of the orogen due mainly to loading and resulting flexure of the lithosphere by the developing mountain belt. |
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The depth, shape and size of a basin depend on tectonics, movements within the Earth's lithosphere. |
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When the lithosphere keeps subsiding, new accommodation space keeps being created. |
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Due to divergent movement, the lithosphere is stretched and thinned, so that the hot asthenosphere rises and heats the overlying rift basin. |
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When the basin grows due to continued stretching of the lithosphere, the rift grows and the sea can enter, forming marine deposits. |
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When a piece of lithosphere that was heated and stretched cools again, its density rises, causing isostatic subsidence. |
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Earth's lithosphere is divided into several rigid tectonic plates that migrate across the surface over periods of many millions of years. |
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The mechanically rigid outer layer of Earth, the lithosphere, is divided into pieces called tectonic plates. |
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The crust and the relatively rigid peridotite below it make up the oceanic lithosphere. |
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This bulge is thought to be caused by upward convective forces in the asthenosphere pushing the oceanic crust and lithosphere. |
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The oceanic lithosphere in the area is directly related to the opening of the North Atlantic Ocean and one of the oldest preserved on Earth. |
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When oceanic plates diverge, tensional stress causes fractures to occur in the lithosphere. |
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In this model, the seabed height is determined by the oceanic lithosphere temperature, due to thermal expansion. |
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A passive margin is the transition between oceanic and continental lithosphere that is not an active plate margin. |
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A passive margin forms by sedimentation above an ancient rift, now marked by transitional lithosphere. |
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The transition between the continental and oceanic lithosphere that was originally created by rifting is known as a passive margin. |
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This refers to whether a crustal boundary between oceanic lithosphere and continental lithosphere is a plate boundary or not. |
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While a weld between oceanic and continental lithosphere is called a passive margin, it is not an inactive margin. |
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The lithosphere beneath passive margins is known as transitional lithosphere. |
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The very thin lithosphere beneath the rift allows the upwelling mantle to melt by decompression. |
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Heating reduces the density of the lithosphere and elevates the lower crust and lithosphere. |
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In addition, mantle plumes may heat the lithosphere and cause prodigious igneous activity. |
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The accumulation of sediments above the subsiding transitional crust and lithosphere further depresses the transitional crust. |
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The great thickness of the lithosphere requires that this bending be gentle. |
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These form where fluids released from the downgoing plate percolate upwards and interact with cold mantle lithosphere of the forearc. |
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To say that the lithosphere floats on top of the asthenosphere suggests a degree of easy buoyancy that isn't quite right. |
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A second order control on trench depth is the age of the lithosphere at the time of subduction. |
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The subduction process consumes older oceanic lithosphere, so oceanic crust is seldom more than 200 million years old. |
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Seamounts provide data on movements of tectonic plates on which they ride, and on the rheology of the underlying lithosphere. |
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The remainder appear to originate in the upper mantle and have been suggested to result from the breakup of subducting lithosphere. |
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This is because the age of the oceanic lithosphere provides a major control on the depth of the ocean basins, and therefore on global sea level. |
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That is, the subducted lithosphere is always oceanic while the overriding lithosphere may or may not be oceanic. |
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Subduction zones exist at convergent plate boundaries where one plate of oceanic lithosphere converges with another plate. |
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It is at subduction zones that Earth's lithosphere, oceanic crust, sedimentary layers and some trapped water are recycled into the deep mantle. |
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Seismic tomography has helped detect subducted lithosphere in regions where there are no earthquakes. |
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The thick lithosphere predicted by these models appears to be inconsistent with even a low level of ongoing volcanism and tectonism. |
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The lithosphere likes to float on the aesthenosphere, the soft mobile voice of the unseen. |
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Most of this water is trapped in pores and fractures in the upper lithosphere and sediments of the subducting plate. |
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Transform faults are also referred to as conservative plate boundaries, as lithosphere is neither created nor destroyed. |
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A fault that passes through different levels of the lithosphere will have many different types of fault rock developed along its surface. |
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The weight of the redistributed surface mass loaded the lithosphere, caused it to flex and also induced stress within the Earth. |
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Water is driven out of the oceanic lithosphere in subduction zones, and it causes melting in the overlying mantle. |
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Temperature increases also may contribute to the melting of lithosphere dragged down in a subduction zone. |
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A rift is a region where the lithosphere extends as two parts of the Earth's crust pull apart. |
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As the rift expands, the rift flanks lift up due to isostatic compensation of the lithosphere. |
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Continents sit on continental lithosphere which is part of tectonic plates floating high on Earth's mantle. |
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Oceanic crust is also part of tectonic plates, but it is denser than continental lithosphere, so it floats low on the mantle. |
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This holds true for Australia, which sits on its own continental lithosphere and tectonic plate. |
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In geology, a rift is a linear zone where the lithosphere is being pulled apart and is an example of extensional tectonics. |
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Segment lengths vary between rifts, depending on the elastic thickness of the lithosphere. |
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At the same time, the mantle lithosphere becomes thinned, causing a rise of the top of the asthenosphere. |
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Deformation of continental lithosphere can take place in several possible modes. |
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During the first stage, the oceanic lithosphere subducted from NE to SW under the subcontinental crust. |
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This vertical stress is supported by the mantle and the flexure of the lithosphere. |
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Tectonic plates are composed of oceanic lithosphere and thicker continental lithosphere, each topped by its own kind of crust. |
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Tectonic plates are able to move because the Earth's lithosphere has greater mechanical strength than the underlying asthenosphere. |
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The outer layers of the Earth are divided into the lithosphere and asthenosphere. |
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Tomographic images of the Iberian subcrustal lithosphere and asthenosphere. |
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These reactions generate and define endogeny, their silicon furnishing the basis for continental shields and lithosphere generally. |
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Environment refers to everything that surrounds us and consists of the lithosphere, hydrosphere, atmosphere, and biosphere. |
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Because oceanic lithosphere cools and thickens as it ages, it subsides. |
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The mantle lithosphere below the thinned and faulted continental oceanic transition cools, thickens, increases in density and thus begins to subside. |
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Lithospheric thinning also allows the asthenosphere to rise closer to the surface, heating the overlying lithosphere by conduction and advection of heat by intrusive dykes. |
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The lithosphere thins seaward as it transitions seaward to oceanic crust. |
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In the smooth areas the lithosphere is more magmatic in composition. |
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Current research indicates that complex convection within the Earth's mantle allows material to rise to the base of the lithosphere beneath each divergent plate boundary. |
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The crust and the cold, rigid, top of the upper mantle are collectively known as the lithosphere, and it is of the lithosphere that the tectonic plates are composed. |
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This volcanic arc was formed above a subduction zone where the oceanic lithosphere of the Iapetus Ocean subducted southward under other oceanic lithosphere. |
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What exactly happens in a specific orogen depends upon the strength and rheology of the continental lithosphere, and how these properties change during orogenesis. |
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Geologists attribute the arcuate structure to the rigidity of the descending plate, and island arc cusps relate to tears in the descending lithosphere. |
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Major isostatic adjustments of the lithosphere during the Quaternary glaciation were caused by the weight of the ice, which depressed the continents. |
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Abyssal hills are formed by stretching of the oceanic lithosphere. |
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It has generally been accepted that tectonic plates are able to move because of the relative density of oceanic lithosphere and the relative weakness of the asthenosphere. |
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In this way, the total surface of the lithosphere remains the same. |
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Although volcanoes are technically part of the lithosphere, which itself is part of the climate system, the IPCC explicitly defines volcanism as an external forcing agent. |
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The Earth's outer solid layer, the lithosphere, is made of rock. |
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Since the mantle and the lithosphere continuously respond to the changing ice and water loads, the state of stress at any location continuously changes in time. |
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At the onset of rifting, the upper part of the lithosphere starts to extend on a series of initially unconnected normal faults, leading to the development of isolated basins. |
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Where the oceanic crust is subducted under a continental plate sediments will be carried down to warmer zones in the asthenosphere and lithosphere. |
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Atomic mass of an element in Table of Elements is presented by the average atomic mass of all stable isotopes of the element with taking their content in the lithosphere. |
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Relative depth may be controlled by the age of the lithosphere at the trench, the convergence rate, and the dip of the subducted slab at intermediate depths. |
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