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Slab

About: Slab is a research topic. Over the lifetime, 31617 publications have been published within this topic receiving 318693 citations.


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Journal ArticleDOI
11 Mar 1999-Nature
TL;DR: In this article, the authors proposed a model for subduction-zone magmatism, where non-percolating water provides the high pore-pressure, that the consequent faulting temporarily interconnects the water pores and, when a sufficient vertical height of water is interconnected, a hydrofracture is produced which transports the water out into the mantle wedge, thereby generating subductionzone magnetism.
Abstract: The presence of magmatism and intermediate-depth (70–300 km deep) seismicity at subduction zones is at first sight surprising. Magmatism is unexpected because the subduction of cool oceanic lithosphere makes these regions the coldest in the mantle. The current model for subduction-zone magmatism is that water released from the subducting slab enters the relatively warm mantle wedge, leading to a reduction in melting temperature and magmatism1, 2, 3, 4. But there is a problem with this scheme because it is thought that water cannot leave the slab by porous flow to enter the wedge. The occurrence of intermediate-depth earthquakes is surprising because of the inhibitory effect of the very high frictional stress on faults expected from the high pressure at these depths. One proposal put forward to explain intermediate-depth seismicity is that high pore-pressure might facilitate faulting by decreasing the friction5, 6, 7. The hypothesis presented here is that non-percolating water provides the high pore-pressure, that the consequent faulting temporarily interconnects the water pores and, when a sufficient vertical height of water is interconnected, a hydrofracture is produced which transports the water out into the mantle wedge, thereby generating subduction-zone magmatism.

161 citations

Journal ArticleDOI
TL;DR: In this paper, the authors examined the thermal effects of mantle flow induced by traction along the top of the subducting plate and showed that the model thermal structure of the wedge is primarily determined by the assumed temperatures along this boundary.

160 citations

Journal ArticleDOI
TL;DR: In this paper, the results of an experimental program aimed to investigate a number of different mechanical "dry-dry" connectors previously embedded into a prefabricated concrete slab were performed.
Abstract: Timber–concrete composite beams and slabs require interlayer connectors, which provide composite action in the cross-section. A range of mechanical connectors is available on the market with an extensive variety of stiffness and strength properties, which are fundamental design parameters for the composite structure. Another crucial parameter is the cost of the connector, including the labour cost, that if too high may prevent the use of the composite system. In order to reduce the construction cost and make timber–concrete structures more widespread on the market, it is believed that a high degree of prefabrication should be achieved. For a simple and cost effective construction process, the use of “dry” connections, which do not require the pouring and curing of concrete on site, may represent a possible solution. This paper reports the outcomes of an experimental programme aimed to investigate a number of different mechanical “dry–dry” connectors previously embedded into a prefabricated concrete slab. Direct shear tests on small blocks made of a glulam segment connected with a prefabricated concrete slab were performed. The shear force-relative slip relationships were measured and all the relevant mechanical properties such as slip moduli and shear strengths were calculated. It was found that some of the new developed connection systems for prefabricated concrete slab can perform as satisfactorily as those for cast-in-situ slabs, with the additional benefit of being relatively inexpensive.

160 citations

Journal ArticleDOI
TL;DR: In this article, it was shown that phase transformations play a major role in driving the lithosphere slab into the mantle at depths greater than 300 km, and also control the stress distribution within the slab.

160 citations

Journal ArticleDOI
TL;DR: In this paper, the authors investigate the dynamics and energy properties of a free subduction system driven solely by downgoing plate buoyancy, using a finite-element model of a viscoelastic plate with a free surface, sinking into a passive unbounded mantle represented by drag forces.

159 citations


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Performance
Metrics
No. of papers in the topic in previous years
YearPapers
20242
20231,170
20222,180
2021774
20201,133
20191,317