| scholarly article | Q13442814 |
| P819 | ADS bibcode | 2012GGG....13.1010F |
| P356 | DOI | 10.1029/2011GC003860 |
| P50 | author | Louis Moresi | Q6687845 |
| Manuele Faccenda | Q90105570 | ||
| P2093 | author name string | Taras V. Gerya | |
| Neil S. Mancktelow | |||
| P2860 | cites work | Rheology of the upper mantle: a synthesis | Q28243293 |
| Whole-mantle convection and the transition-zone water filter | Q34227876 | ||
| A chronology of Paleozoic sea-level changes | Q34844270 | ||
| Seismic evidence for sharp lithosphere-asthenosphere boundaries of oceanic plates | Q34977517 | ||
| The dynamics of melt and shear localization in partially molten aggregates | Q42015701 | ||
| Intermediate-depth earthquake faulting by dehydration embrittlement with negative volume change | Q46721003 | ||
| Evolution and diversity of subduction zones controlled by slab width. | Q55043602 | ||
| Subduction factory 2. Are intermediate-depth earthquakes in subducting slabs linked to metamorphic dehydration reactions? | Q56136855 | ||
| Deep seismic structure of the Tonga subduction zone: Implications for mantle hydration, tectonic erosion, and arc magmatism | Q56235203 | ||
| H2O subduction beyond arcs | Q56454029 | ||
| Global prevalence of double Benioff zones | Q57118031 | ||
| A periodic shear-heating mechanism for intermediate-depth earthquakes in the mantle | Q57118344 | ||
| Bending-related faulting and mantle serpentinization at the Middle America trench | Q57124694 | ||
| Trench-parallel fast axes of seismic anisotropy due to fluid-filled cracks in subducting slabs | Q57737656 | ||
| High-resolution subducting-slab structure beneath northern Honshu, Japan, revealed by double-difference tomography | Q57820343 | ||
| Serpentinization in the trench-outer rise region offshore of Nicaragua: constraints from seismic refraction and wide-angle data | Q57855140 | ||
| Signatures of downgoing plate-buoyancy driven subduction in Cenozoic plate motions | Q57866384 | ||
| Dynamics of plate bending at the trench and slab-plate coupling | Q57866405 | ||
| Dynamic models of downgoing plate-buoyancy driven subduction: Subduction motions and energy dissipation | Q57866416 | ||
| Earthquakes and plastic deformation of anhydrous slab mantle in double Wadati-Benioff zones | Q57869792 | ||
| Why is terrestrial subduction one-sided? | Q58210869 | ||
| Fault-induced seismic anisotropy by hydration in subducting oceanic plates | Q59051531 | ||
| The effect of water on the electrical conductivity of olivine | Q59056924 | ||
| Recycled dehydrated lithosphere observed in plume-influenced mid-ocean-ridge basalt | Q59096356 | ||
| Experimentally based water budgets for dehydrating slabs and consequences for arc magma generation | Q59405616 | ||
| Controls on back-arc basin formation | Q59794995 | ||
| Seismic tomography and earthquake locations in the Nicaraguan and Costa Rican upper mantle | Q60118036 | ||
| Water flow to the mantle transition zone inferred from a receiver function image of the Pacific slab | Q60708729 | ||
| Tomographic imaging of hydrated crust and mantle in the subducting Pacific slab beneath Hokkaido, Japan: Evidence for dehydration embrittlement as a cause of intraslab earthquakes | Q60720003 | ||
| Double seismic zone and dehydration embrittlement of the subducting slab | Q61834976 | ||
| Serpentine and the subduction zone water cycle | Q64013030 | ||
| Double-Difference Tomography: The Method and Its Application to the Hayward Fault, California | Q98753427 | ||
| Antigorite: High-pressure stability in the system MgOSiO2H2O (MSH) | Q98962714 | ||
| P433 | issue | 1 | |
| P921 | main subject | fluid flow | Q12142910 |
| P577 | publication date | 2012-01-01 | |
| P1433 | published in | G3: Geochemistry, Geophysics, Geosystems | Q15759647 |
| P1476 | title | Fluid flow during slab unbending and dehydration: Implications for intermediate-depth seismicity, slab weakening and deep water recycling | |
| P478 | volume | 13 |
| Q58876109 | Chlorine isotope constraints on fluid-rock interactions during subduction and exhumation of the Zermatt-Saas ophiolite |
| Q43528363 | Continental flood basalts derived from the hydrous mantle transition zone. |
| Q57855081 | Controls of faulting and reaction kinetics on serpentinization and double Benioff zones |
| Q106465216 | Deep Water Cycling and Sea Level Change Since the Breakup of Pangea |
| Q38686786 | Dehydration of subducting slow-spread oceanic lithosphere in the Lesser Antilles |
| Q60697962 | Evidence for Rupture Through a Double Benioff Zone During the 2017 M w 8.2 Chiapas, Mexico Earthquake |
| Q97667635 | Intermediate-Depth Earthquakes Controlled by Incoming Plate Hydration Along Bending-Related Faults |
| Q57866355 | Seismic anisotropy around subduction zones: Insights from three-dimensional modeling of upper mantle deformation and SKS splitting calculations |
| Q98222135 | Subduction hides high-pressure sources of energy that may feed the deep subsurface biosphere |
| Q59068615 | Water input into the Mariana subduction zone estimated from ocean-bottom seismic data |
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