| scholarly article | Q13442814 |
| P819 | ADS bibcode | 2014Natur.510..389A |
| P6179 | Dimensions Publication ID | 1051978263 |
| P356 | DOI | 10.1038/NATURE13391 |
| P2888 | exact match | https://scigraph.springernature.com/pub.10.1038/nature13391 |
| P698 | PubMed publication ID | 24943955 |
| P50 | author | Roland Bürgmann | Q58024297 |
| Pascal Audet | Q88046487 | ||
| P2860 | cites work | Resonant slow fault slip in subduction zones forced by climatic load stress | Q40296926 |
| Low-frequency earthquakes in Shikoku, Japan, and their relationship to episodic tremor and slip | Q40307708 | ||
| Seismic evidence for overpressured subducted oceanic crust and megathrust fault sealing. | Q50276034 | ||
| Dilatant strengthening as a mechanism for slow slip events | Q56997252 | ||
| The role of crustal quartz in controlling Cordilleran deformation | Q57109864 | ||
| Subducting slab ultra-slow velocity layer coincident with silent earthquakes in southern Mexico | Q57114780 | ||
| High pore pressures and porosity at 35 km depth in the Cascadia subduction zone | Q58081998 | ||
| Segmentation in episodic tremor and slip all along Cascadia | Q58222342 | ||
| Slow slip events in Mexico revised from the processing of 11 year GPS observations | Q59189640 | ||
| Annual modulation of non-volcanic tremor in northern Cascadia | Q59805094 | ||
| Pole-Tide Modulation of Slow Slip Events at Circum-Pacific Subduction Zones | Q59805850 | ||
| Slow slip events in Costa Rica detected by continuous GPS observations, 2002-2011 | Q59875720 | ||
| Slow Earthquakes and Nonvolcanic Tremor | Q60162536 | ||
| Slab1.0: A three-dimensional model of global subduction zone geometries | Q60957858 | ||
| Slab morphology in the Cascadia fore arc and its relation to episodic tremor and slip | Q62019483 | ||
| Weakening of the subduction interface and its effects on surface heat flow, slab dehydration, and mantle wedge serpentinization | Q96679085 | ||
| The solubility of quartz in H2O in the lower crust and upper mantle | Q116225669 | ||
| P433 | issue | 7505 | |
| P407 | language of work or name | English | Q1860 |
| P921 | main subject | earthquake | Q7944 |
| subduction zone | Q4493162 | ||
| P304 | page(s) | 389-392 | |
| P577 | publication date | 2014-06-01 | |
| P1433 | published in | Nature | Q180445 |
| P1476 | title | Possible control of subduction zone slow-earthquake periodicity by silica enrichment | |
| P478 | volume | 510 |
| Q57093062 | Back to full interseismic plate locking decades after the giant 1960 Chile earthquake |
| Q59804954 | Diary of a wimpy fault |
| Q38667178 | Discontinuous boundaries of slow slip events beneath the Bungo Channel, southwest Japan |
| Q101248732 | Dynamically Triggered Changes of Plate Interface Coupling in Southern Cascadia |
| Q63947102 | Earthquakes track subduction fluids from slab source to mantle wedge sink |
| Q59830639 | Fluid Controls on the Heterogeneous Seismic Characteristics of the Cascadia Margin |
| Q57852243 | Fluid-controlled deformation in blueschist-facies conditions: plastic vs brittle behaviour in a brecciated mylonite (Voltri Massif, Western Alps, Italy) |
| Q60704681 | High‐Resolution Receiver Function Imaging Across the Cascadia Subduction Zone Using a Dense Nodal Array |
| Q57869660 | Mantle hydration and Cl-rich fluids in the subduction forearc |
| Q55155105 | Revealing the cluster of slow transients behind a large slow slip event. |
| Q50240465 | Rheological separation of the megathrust seismogenic zone and episodic tremor and slip. |
| Q89498377 | Seismic evidence for megathrust fault-valve behavior during episodic tremor and slip |
| Q42684149 | Silica precipitation potentially controls earthquake recurrence in seismogenic zones |
| Q91622978 | Stress-driven fluid flow controls long-term megathrust strength and deep accretionary dynamics |
| Q98284520 | Structural Heterogeneity in Source Zones of the 2018 Anchorage Intraslab Earthquake and the 1964 Alaska Megathrust Earthquake |
| Q39922967 | Tremor activity inhibited by well-drained conditions above a megathrust. |
| Q60697728 | Using Tectonic Tremor to Constrain Seismic Wave Attenuation in Cascadia |
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