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词汇 example_english_plate-tectonics
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Examples of plate tectonics


These examples are from corpora and from sources on the web. Any opinions in the examples do not represent the opinion of the Cambridge Dictionary editors or of Cambridge University Press or its licensors.
Subduction of dense cold plates into the mantle leads to platetectonics.
The requirements for platetectonics of water and mass are also independently requirements for habitable planets.
So these requirements for platetectonics are already fundamental conditions for a habitable planet.
If platetectonics occurs, it must involve crustal fractionation into components with different buoyancy.
The model is based on the global carbon cycle mediated by life and driven by increasing stellar luminosity and platetectonics.
The likelihood of platetectonics is difficult to predict.
In other words, the incidence of platetectonics on a planet which we identify as potentially habitable could be quite high.
In this paper we speculate on how platetectonics influences surface mineralogy, and identify three examples which could influence the development of life.
A third choice would be to focus on the time before platetectonics, a time that is poorly understood and hard to specify.
There are a number of exercises new to this edition using the new technology outlined above to illustrate concepts associated with platetectonics.
The last six chapters cover more advanced topics: rheological models, brittle failure, strain measurement, balanced cross sections, deformation mechanisms, and the geometry of platetectonics.
The issues under discussion have evolved not analogous to platetectonics in a slow, orderly pattern, but more like a volcanic explosion.
Particularly provoking is a chapter on future platetectonics with scenarios for time periods from +50 to +200 million years ahead.
This was confirmed by palaeomagnetic research almost 34 years later, once the theory of platetectonics had been firmly established.
The third chapter introduces platetectonics in a thoroughly confusing way.
Recycling is powered and controlled by platetectonics.
But even if mass and water are present to enhance the possibility of platetectonics, there are other variables.
This brief paper adds to the known significance of platetectonics in creating a habitable planet.
Irrefutable evidence, as in the classic case of platetectonics, can also resolve scientific disagreements, but is usually accompanied by much rancor before one side finally concedes.
Conditions for the onset of platetectonics on terrestrial planets and moons.
The zone of liquid water has a more restricted distribution than the distribution of planets of adequate size, so is the greater constraint on the likelihood of platetectonics.
The generation of platetectonics from mantle convection.
Fundamental uncertainties arise both with the sequence of geodynamic processes that eventually lead to the triumph of platetectonics and life and with the timing of events.
In large part this evolution reflects the overriding influence of platetectonics and the interconnected effects of tectonics, uplift, and denudation on local, regional and global scales.
In contrast, the photic zone in quartzose sediments would, as a consequence of platetectonics, reach beneath the influence of harmful irradiation and provide a niche for photosynthesis.
Orogenic andesites and platetectonics.
An application of platetectonics.
This paleolatitude is affected both by true polar wander and by platetectonics.
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This idea was used to help bolster the theory of platetectonics.
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A large satellite also increases the likelihood of platetectonics through the effect of tidal forces on the planet's crust.
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Nontheistic models predict that evidence for fine-tuned, long-lasting platetectonics will weaken as scientists learn more about plate tectonic phenomena.
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Before the advent of platetectonics in the early 1970s, it was difficult to explain mlanges in terms of known geological mechanisms.
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Lessons include seasons, photosynthesis, erosion, the rock cycle and platetectonics.
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The surface features built up or deformed through platetectonics are subject to steady weathering from precipitation, thermal cycles, and chemical effects.
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Tyson then explains on the nature of platetectonics that would shape the landmasses of the world.
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His theories have few supporters in the geological community compared to the more widely accepted model of platetectonics.
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Platetectonics also provided a unified explanation for a wide range of seemingly unrelated geological phenomena.
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The resulting process is known as platetectonics.
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Sea level changes are mostly due to glaciation or platetectonics.
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These processes are associated with large-scale movements of the earth's crust (platetectonics).
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These ideas had to be adjusted with platetectonics as the mechanism of orogeny.
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How did the planet cool down before platetectonics?
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The dataset can be used to teach different topics, such as natural hazards, solid earth, platetectonics, etc. in geophysics and structural geology.
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This information can be used to provide insights into platetectonics, mantle convection, the geodynamo and related phenomena.
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His research expertise encompasses massive volcanism on the seafloor, environmental effects of massive volcanism, platetectonics, and rifted continental margins.
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Seafloor spreading helps explain continental drift in the theory of platetectonics.
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The use of this data has resulted in evidence for continental drift, platetectonics and supercontinents.
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Ice ages may occur because of changes in ocean circulation and continentality induced by platetectonics.
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The second floor contains exhibits focusing on earth sciences, including platetectonics, rock formation and precious gems.
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These change only over periods of millions of years due to processes such as platetectonics.
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At this point he decided to move away from platetectonics, choosing instead to focus on the behavior of fluids below the plates.
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As a likely consequence, platetectonics will come to an end.
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This is considered a classic publication in the history of platetectonics theory.
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Such plumes were invoked in 1971 to explain volcanic regions that were not thought to be explicable by the then-new theory of platetectonics.
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Among many other contributions, he is known for his comprehensive model of platetectonics (1968).
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Volcanic anomalies are created by platetectonics such as spreading plate boundaries or subduction zones.
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Platetectonics is a theory developed during the 1960s which describes the movement of continents by way of the separation and collision of crustal plates.
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Due to platetectonics, these areas were at that time less than 1500 km apart rather than the 4000 km of today.
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The active mode of platetectonics occurs when the thick lithosphere detaches and founders into the interior of the planet.
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These earthquakes are unique in that they are not associated with platetectonics.
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With the developing understanding of the driving "engine" of platetectonics, the rock cycle changed from endlessly repetitive to a gradually evolving process.
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The broad fault-block mountain is characteristic of the basin and range platetectonics of the high desert.
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It encompasses the history of navigation using compasses, studies of the prehistoric magnetic field (archeomagnetism and paleomagnetism), and applications to platetectonics.
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The locations of earthquakes provide information on platetectonics and mantle convection.
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Subduction is the driving force behind platetectonics, and without it platetectonics could not occur.
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Platetectonics also provided the mechanism by which the former ocean disappeared.
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Earth's internal heat powers most geological processes and drives platetectonics.
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Discovery in all its many forms are present - exploration, scientific, medical, mathematical and the more theoretical ones such as time, evolution, platetectonics and relativity.
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In keeping with her interest in the natural environment, the clay slab method closely mimics geological phenomena, including platetectonics.
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Menard is perhaps best known for his promotion of the theory of platetectonics before it was widely accepted in the scientific community.
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Such information in turn is helpful in studying the motions of continents and ocean floors in the process of platetectonics.
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Earth may in fact lie on the lower boundary of habitability: if it were any smaller, platetectonics would be impossible.
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Over this short time period, there has been relatively little change in the distribution of the continents due to platetectonics.
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This work was a major step in the development of platetectonics.
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The sinking of cold lithosphere at subduction zones is another example of downwelling in platetectonics.
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Answers can again be inferred using the finite size of the world's plates (platetectonics), and the possible limits of the various magnitude scales.
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This extended our understanding of the dynamic processes involved in platetectonics.
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The magmatic aspects of platetectonics tends to gradual segregation within or between the mantle and crust.
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This concept of a repetitive non-evolutionary rock cycle remained dominant until the platetectonics revolution of the 1960s.
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The key principle of platetectonics is that the lithosphere exists as separate and distinct tectonic plates, which ride on the fluid-like (visco-elastic solid) asthenosphere.
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Continents formed by platetectonics, a process ultimately driven by the continuous loss of heat from the earth's interior.
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It is thought that the platetectonics of the area are adding to the height and moving the summit northeastwards.
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He was the author of two books on platetectonics and over a hundred scientific papers.
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Of the many forces discussed in this paragraph, tidal force is still highly debated and defended as a possible principle driving force of platetectonics.
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This is called a divergent platetectonics boundary.
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Paleomagnetism continues to extend the history of platetectonics back in time and are applied to the movement of continental fragments, or terranes.
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Its liquid hydrosphere is unique among the terrestrial planets, and it is the only planet where platetectonics has been observed.
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This useful synthesis of geological theory persisted until the mid-20th century, but was ultimately supplanted by platetectonics.
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Platetectonics theory arose from two separate geological observations: seafloor spreading and continental drift.
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Topics covered included astrophysics, climatology, geology, glaciology, microbiology, paleobotany, paleontology, palynology, platetectonics, soil remineralization, seismology, soil science, solar physics and human survival.
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Wegener, in 1910, proposed a system of continental drift which was eventually modified and generally accepted as platetectonics.
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Platetectonics are responsible for the uplift of the mountain ranges that cross the park.
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These examples are from corpora and from sources on the web. Any opinions in the examples do not represent the opinion of the Cambridge Dictionary editors or of Cambridge University Press or its licensors.
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