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                    <title>Phys.org news tagged with:mantle convection</title>
            <link>https://phys.org/</link>
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            <description>Phys.org internet news portal provides the latest news on science including: Physics, Nanotechnology, Life Sciences, Space Science, Earth Science, Environment, Health and Medicine.</description>

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                    <title>Research suggests Earth&#039;s oldest continental crust is disintegrating</title>
                    <description>Earth&#039;s continental configurations have changed dramatically over its billions of years&#039; history, transforming not only their positions across the planet, but also their topography as expansion and contraction of the crust made a mark on the landscape. Some areas of continental crust have maintained long-term stability from the beginning of Earth&#039;s history, with little destruction by tectonic events or mantle convection, known as cratons.</description>
                    <link>https://phys.org/news/2024-10-earth-oldest-continental-crust-disintegrating.html</link>
                    <category>Earth Sciences</category>                    <pubDate>Tue, 08 Oct 2024 07:00:01 EDT</pubDate>
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                    <title>Small-scale convection shuffles the oceanic lithosphere, finds study</title>
                    <description>The oceanic lithosphere forms at the summit of ocean ridges during seafloor spreading. Still, the formation of ocean basins is complex, influenced by smaller-scale convection, stagnated pieces of the lithosphere, and tectonic motion from nearby plates. These factors can produce a solid, outer layer of Earth with different structures at different depths.</description>
                    <link>https://phys.org/news/2023-02-small-scale-convection-shuffles-oceanic-lithosphere.html</link>
                    <category>Earth Sciences</category>                    <pubDate>Tue, 21 Feb 2023 12:22:03 EST</pubDate>
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                    <title>Earth&#039;s interior is cooling faster than expected</title>
                    <description>Researchers at ETH Zurich have demonstrated in the lab how well a mineral common at the boundary between the Earth&#039;s core and mantle conducts heat. This leads them to suspect that the Earth&#039;s heat may dissipate sooner than previously thought.</description>
                    <link>https://phys.org/news/2022-01-earth-interior-cooling-faster.html</link>
                    <category>Earth Sciences</category>                    <pubDate>Fri, 14 Jan 2022 08:20:41 EST</pubDate>
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                    <title>Slow start of plate tectonics despite a hot early Earth</title>
                    <description>Writing in PNAS, scientists from Cologne university present important new constraints showing that plate tectonics started relatively slow, although the early Earth&#039;s interior was much hotter than today.</description>
                    <link>https://phys.org/news/2020-12-plate-tectonics-hot-early-earth.html</link>
                    <category>Earth Sciences</category>                    <pubDate>Tue, 22 Dec 2020 12:21:07 EST</pubDate>
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                    <title>A wrench in Earth&#039;s engine</title>
                    <description>Researchers at CU Boulder report that they may have solved a geophysical mystery, pinning down the likely cause of a phenomenon that resembles a wrench in the engine of the planet.</description>
                    <link>https://phys.org/news/2018-10-wrench-earth.html</link>
                    <category>Earth Sciences</category>                    <pubDate>Mon, 01 Oct 2018 16:11:11 EDT</pubDate>
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                    <title>Scientists ID three causes of Earth&#039;s spin axis drift</title>
                    <description>A typical desk globe is designed to be a geometric sphere and to rotate smoothly when you spin it. Our actual planet is far less perfect—in both shape and in rotation.</description>
                    <link>https://phys.org/news/2018-09-scientists-id-earth-axis-drift.html</link>
                    <category>Earth Sciences</category>                    <pubDate>Thu, 20 Sep 2018 08:19:30 EDT</pubDate>
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                    <title>Unusual thermal convection in a well-mixed fluid</title>
                    <description>Researchers from Tokyo Metropolitan University, have recently discovered unusual thermal convection in a uniform mixture of high- and low-viscosity liquids. Kobayashi and Kurita found that concentration fluctuations are enhanced by thermal convection when the two liquids have a large viscosity difference. Such mixtures are ubiquitously observed in nature, daily life, and manufacturing processes e.g. mantle convection, syrup, polymer products. These results promise further insight into non-equilibrium phenomena in fluid mixtures with contrasting &quot;thickness.&quot;</description>
                    <link>https://phys.org/news/2017-12-unusual-thermal-convection-well-mixed-fluid.html</link>
                    <category>Soft Matter</category>                    <pubDate>Fri, 15 Dec 2017 07:04:50 EST</pubDate>
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                    <title>Research reveals the scale at which Earth&#039;s mantle composition varies</title>
                    <description>New research by Brown University geochemists provides new insights on the scale at which Earth&#039;s mantle varies in chemical composition. The findings could help scientists better understand the mixing process of mantle convection, the slow churning that drives the movement of Earth&#039;s tectonic plates.</description>
                    <link>https://phys.org/news/2017-11-reveals-scale-earth-mantle-composition.html</link>
                    <category>Earth Sciences</category>                    <pubDate>Thu, 23 Nov 2017 05:30:02 EST</pubDate>
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                    <title>Ancient Earth&#039;s hot interior created &#039;graveyard&#039; of continental slabs</title>
                    <description>Plate tectonics has shaped the Earth&#039;s surface for billions of years: Continents and oceanic crust have pushed and pulled on each other, continually rearranging the planet&#039;s façade. As two massive plates collide, one can give way and slide under the other in a process called subduction. The subducted slab then slips down through the Earth&#039;s viscous mantle, like a flat stone through a pool of honey.</description>
                    <link>https://phys.org/news/2017-08-ancient-earth-hot-interior-graveyard.html</link>
                    <category>Earth Sciences</category>                    <pubDate>Tue, 22 Aug 2017 06:46:29 EDT</pubDate>
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                    <title>Geoscientists find explanation for puzzling pockets of rock deep in Earth&#039;s mantle</title>
                    <description>A team led by geoscientists from Arizona State University and Michigan State University has used computer modeling to explain how pockets of mushy rock accumulate at the boundary between Earth&#039;s core and mantle.</description>
                    <link>https://phys.org/news/2017-08-geoscientists-explanation-puzzling-pockets-deep.html</link>
                    <category>Earth Sciences</category>                    <pubDate>Wed, 02 Aug 2017 05:00:02 EDT</pubDate>
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                    <title>Whole-mantle convection with tectonic plates preserves long-term global patterns of upper mantle geochemistry</title>
                    <description>New insights into the convection patterns of the Earth&#039;s mantle and its chemical makeup have been revealed by a researcher from the University of Leicester.</description>
                    <link>https://phys.org/news/2017-05-whole-mantle-convection-tectonic-plates-long-term.html</link>
                    <category>Earth Sciences</category>                    <pubDate>Fri, 12 May 2017 08:23:12 EDT</pubDate>
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                    <title>New model for deep mantle conveyor belt system at the core of the Earth</title>
                    <description>Geophysicists at the Earth-Life Science Institute (ELSI) at the Tokyo Institute of Technology report in Nature Geoscience a new model for the existence of a deep mantle conveyor belt system that may have operated inside the Earth since its formation about 4.5 billion years ago.</description>
                    <link>https://phys.org/news/2017-02-deep-mantle-conveyor-belt-core.html</link>
                    <category>Earth Sciences</category>                    <pubDate>Tue, 28 Feb 2017 06:35:48 EST</pubDate>
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                    <title>Heat from Earth&#039;s core could be underlying force in plate tectonics</title>
                    <description>For decades, scientists have theorized that the movement of Earth&#039;s tectonic plates is driven largely by negative buoyancy created as they cool. New research, however, shows plate dynamics are driven significantly by the additional force of heat drawn from the Earth&#039;s core.</description>
                    <link>https://phys.org/news/2017-01-earth-core-underlying-plate-tectonics.html</link>
                    <category>Earth Sciences</category>                    <pubDate>Wed, 18 Jan 2017 06:48:57 EST</pubDate>
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                    <title>A new Goldilocks for habitable planets</title>
                    <description>The search for habitable, alien worlds needs to make room for a second &quot;Goldilocks,&quot; according to a Yale University researcher.</description>
                    <link>https://phys.org/news/2016-08-goldilocks-habitable-planets.html</link>
                    <category>Astronomy</category>                    <pubDate>Fri, 19 Aug 2016 15:08:24 EDT</pubDate>
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                    <title>Scientists crack mystery of the Sierra Nevada&#039;s age</title>
                    <description>In science, the simplest questions often prove themselves the most difficult to answer. Questions such as what killed the dinosaurs, or how many fish are there in the oceans took decades to solve or remain unanswered.</description>
                    <link>https://phys.org/news/2015-12-scientists-mystery-sierra-nevada-age.html</link>
                    <category>Earth Sciences</category>                    <pubDate>Mon, 14 Dec 2015 06:25:48 EST</pubDate>
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                    <title>Twin studies provide first explanations for boundary within Earth&#039;s mantle</title>
                    <description>Earth&#039;s mantle, the large zone of slow-flowing rock that lies between the crust and the planet&#039;s core, powers every earthquake and volcanic eruption on the planet&#039;s surface. Evidence suggests that the mantle behaves differently below 1 megameter (1,000 kilometers, or 621 miles) in depth, but so far seismologists have not been able to explain why this boundary exists.</description>
                    <link>https://phys.org/news/2015-12-twin-explanations-boundary-earth-mantle.html</link>
                    <category>Earth Sciences</category>                    <pubDate>Thu, 10 Dec 2015 14:00:09 EST</pubDate>
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                    <title>An ammonia-water slurry may swirl below Pluto&#039;s icy surface</title>
                    <description>Researchers propose an ammonia-water slurry as the basis for Pluto&#039;s newly discovered geologic activity and possible volcanism, and offer a new method to predict planetary vigor.</description>
                    <link>https://phys.org/news/2015-11-ammonia-water-slurry-swirl-pluto-icy.html</link>
                    <category>Space Exploration</category>                    <pubDate>Mon, 09 Nov 2015 17:10:19 EST</pubDate>
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                    <title>Ancient deformation of the lithosphere revealed in Eastern China</title>
                    <description>Seismic investigations from the Qinling-Dabie-Sulu orogenic belt in eastern China suggest that this region was affected by extreme mantle perturbation and crust-mantle interaction during the Mesozoic era. The Qinling-Dabie-Sulu orogenic belt formed through the collision between the North and South China blocks, which produced large-scale destruction of the cratonic lithosphere, accompanied by widespread magmatism and metallogeny.</description>
                    <link>https://phys.org/news/2015-01-ancient-deformation-lithosphere-revealed-eastern.html</link>
                    <category>Earth Sciences</category>                    <pubDate>Fri, 30 Jan 2015 17:25:06 EST</pubDate>
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                    <title>New insight into the temperature of deep Earth</title>
                    <description>Scientists from the Magma and Volcanoes Laboratory (CNRS) and the European Synchrotron, the ESRF, have recreated the extreme conditions 600 to 2900 km below the Earth&#039;s surface to investigate the melting of basalt in the oceanic tectonic plates. They exposed microscopic pieces of rock to these extreme pressures and temperatures while simultaneously studying their structure with the ESRF&#039;s extremely powerful X-ray beam.</description>
                    <link>https://phys.org/news/2014-05-insight-temperature-deep-earth.html</link>
                    <category>Earth Sciences</category>                    <pubDate>Thu, 22 May 2014 14:25:32 EDT</pubDate>
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                    <title>Hot mantle drives elevation, volcanism along mid-ocean ridges</title>
                    <description>Scientists have shown that temperature differences deep within Earth&#039;s mantle control the elevation and volcanic activity along mid-ocean ridges, the colossal mountain ranges that line the ocean floor. The findings, published April 4 in the journal Science, shed new light on how temperature in the depths of the mantle influences the contours of the Earth&#039;s crust.</description>
                    <link>https://phys.org/news/2014-04-hot-mantle-elevation-volcanism-mid-ocean.html</link>
                    <category>Earth Sciences</category>                    <pubDate>Thu, 03 Apr 2014 14:10:02 EDT</pubDate>
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                    <title>New model reveals multiple compositional components of Earth&#039;s deep mantle being carried up to the surface</title>
                    <description>Seeking to better understand the composition of the lowermost part of Earth&#039;s mantle, located nearly 2,900 kilometers (1,800 miles) below the surface, a team of Arizona State University researchers has developed new simulations that depict the dynamics of deep Earth. A paper published March 30 in Nature Geoscience reports the team&#039;s findings, which could be used to explain the complex geochemistry of lava from hotspots such as Hawaii.</description>
                    <link>https://phys.org/news/2014-03-reveals-multiple-compositional-components-earth.html</link>
                    <category>Earth Sciences</category>                    <pubDate>Sun, 30 Mar 2014 13:00:14 EDT</pubDate>
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                    <title>Scientist finds topography of Eastern Seaboard muddles ancient sea level changes</title>
                    <description>(Phys.org) —The distortion of the ancient shoreline and flooding surface of the U.S. Atlantic Coastal Plain are the direct result of fluctuations in topography in the region and could have implications on understanding long-term climate change, according to a new study.</description>
                    <link>https://phys.org/news/2013-05-scientist-topography-eastern-seaboard-ancient.html</link>
                    <category>Earth Sciences</category>                    <pubDate>Thu, 16 May 2013 17:27:11 EDT</pubDate>
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                    <title>New results on geo-neutrinos from Borexino</title>
                    <description>(Phys.org) —Borexino is a liquid scintillator detector mainly built for solar neutrino searches. Due to its high level of radiopurity, a worldwide record, Borexino can also detect rare events such as electron-antineutrinos from the interior of the Earth, namely geo-neutrinos.</description>
                    <link>https://phys.org/news/2013-03-results-geo-neutrinos-borexino.html</link>
                    <category>General Physics</category>                    <pubDate>Thu, 14 Mar 2013 08:47:22 EDT</pubDate>
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                    <title>Deep Carbon: Quest underway to discover its quantity, movements, origins and forms in Earth</title>
                    <description>From Earth&#039;s surface to hundreds of kilometers deeper than oilmen drill, the Deep Carbon Observatory (DCO) is investigating the surprising quantity of carbon in the deep, dark Earth beyond photosynthesis.</description>
                    <link>https://phys.org/news/2013-03-deep-carbon-quest-underway-quantity.html</link>
                    <category>Earth Sciences</category>                    <pubDate>Mon, 04 Mar 2013 12:38:18 EST</pubDate>
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                    <title>Magma in Earth&#039;s mantle forms deeper than once thought</title>
                    <description>Magma forms far deeper than geologists previously thought, according to new research results.</description>
                    <link>https://phys.org/news/2013-01-magma-earth-mantle-deeper-thought.html</link>
                    <category>Earth Sciences</category>                    <pubDate>Thu, 24 Jan 2013 10:43:41 EST</pubDate>
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                    <title>Magma in mantle has deep impact: Study suggests rocks melt at a greater depth than once thought</title>
                    <description>Magma forms far deeper than geologists previously thought, according to new research at Rice University.</description>
                    <link>https://phys.org/news/2013-01-magma-mantle-deep-impact-greater.html</link>
                    <category>Earth Sciences</category>                    <pubDate>Wed, 09 Jan 2013 13:00:09 EST</pubDate>
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                    <title>New understanding of Earth&#039;s lithosphere-asthenosphere boundary beneath the Pacific Ocean</title>
                    <description>Scientists have long speculated about why there is a large change in the strength of rocks that lie at the boundary between two layers immediately under Earth&#039;s crust: the lithosphere and underlying asthenosphere. Understanding this boundary is central to our knowledge of plate tectonics and thus the formation and evolution of our planet as we know it today. A new technique for observing this transition, particularly in the portion of Earth&#039;s mantle that lies beneath the Pacific Ocean basin, has led Carnegie and NASA Goddard scientist Nick Schmerr to new insight on the origins of the lithosphere and asthenosphere. His work is published March 23 in Science.</description>
                    <link>https://phys.org/news/2012-03-earth-lithosphere-asthenosphere-boundary-beneath-pacific.html</link>
                    <category>Earth Sciences</category>                    <pubDate>Thu, 22 Mar 2012 14:00:05 EDT</pubDate>
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                    <title>Earth&#039;s mantle: New numerical tool describes rock deformation</title>
                    <description>Although solid, the rocks of the Earth&#039;s mantle deform very slowly. Professor Patrick Cordier&#039;s team at the Materials and Transformation Unit (Universit&amp;#233; Lille, France) has developed a model that makes it possible, over timescales of several million years, to link the deformation of these rocks with mantle convection, the fundamental driver of plate tectonics. Until now, no experimental method in the laboratory had achieved the real conditions of deformation of mantle rocks. By applying this model to magnesium oxide, a solid present in the Earth&#039;s mantle, the scientists were able to show how atomic-scale defects in this mineral could be transmitted on a larger scale and over long periods of time. </description>
                    <link>https://phys.org/news/2012-01-earth-mantle-numerical-tool-deformation.html</link>
                    <category>Earth Sciences</category>                    <pubDate>Tue, 24 Jan 2012 08:01:39 EST</pubDate>
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                    <title>Water in Earth&#039;s mantle key to survival of oldest continents</title>
                    <description>Earth today is one of the most active planets in the Solar System, and was probably even more so during the early stages of its life. Thanks to the plate tectonics that continue to shape our planet&#039;s surface, remnants of crust from Earth&#039;s formative years are rare, but not impossible to find. A paper published in Nature Sept. 2 examines how some ancient rocks have resisted being recycled into Earth&#039;s convecting interior.</description>
                    <link>https://phys.org/news/2010-09-earth-mantle-key-survival-oldest.html</link>
                    <category>Earth Sciences</category>                    <pubDate>Thu, 02 Sep 2010 13:25:27 EDT</pubDate>
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                    <title>Turbulence around heat transport</title>
                    <description>(PhysOrg.com) -- Heat transport in the earth&#039;s mantle and in the atmosphere is probably not as effective as previously thought.</description>
                    <link>https://phys.org/news/2009-12-turbulence.html</link>
                    <category>General Physics</category>                    <pubDate>Thu, 03 Dec 2009 09:40:01 EST</pubDate>
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