His scientific interests lie mostly in Mid-ocean ridge, Mid-Atlantic Ridge, Seafloor spreading, Oceanic core complex and Seismology. His Mid-ocean ridge research is multidisciplinary, incorporating perspectives in Transform fault and Hydrothermal circulation. His Mid-Atlantic Ridge study combines topics in areas such as Magmatism, Fault scarp and Petrology.
His Seafloor spreading study also includes
His primary scientific interests are in Hydrothermal circulation, Geochemistry, Seismology, Seafloor spreading and Mid-Atlantic Ridge. His Seismology study frequently intersects with other fields, such as Ridge. Javier Escartín combines subjects such as Magma chamber, Mid-ocean ridge, Petrology, Bathymetry and Oceanic crust with his study of Seafloor spreading.
His Mid-ocean ridge research incorporates elements of Lava, Magmatism, Lithosphere and Magma. The study incorporates disciplines such as Magnetic anomaly and Crust in addition to Mid-Atlantic Ridge. The Fault scarp research Javier Escartín does as part of his general Fault study is frequently linked to other disciplines of science, such as Oceanic core complex, therefore creating a link between diverse domains of science.
His main research concerns Seismology, Seafloor spreading, Fault, Geochemistry and Submarine. His Tectonics, Mass wasting, Induced seismicity and Landslide study in the realm of Seismology connects with subjects such as Fault model. The various areas that he examines in his Seafloor spreading study include Tectonophysics, Seabed, Petrology, Bathymetry and Oceanic crust.
The Petrology study combines topics in areas such as Ridge and Mid-ocean ridge. His work on Fault scarp, Cataclastic rock and Fault breccia as part of general Fault study is frequently linked to Oceanic core complex, bridging the gap between disciplines. Javier Escartín interconnects Hydrothermal circulation and Geomorphology in the investigation of issues within Geochemistry.
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Corrugated slip surfaces formed at ridge–transform intersections on the Mid-Atlantic Ridge
J. R. Cann;D. K. Blackman;D. K. Smith;E. McAllister.
Nature (1997)
Central role of detachment faults in accretion of slow-spreading oceanic lithosphere
Javier E. Escartin;Deborah K. Smith;Johnson R. Cann;Hans A. Schouten.
Nature (2008)
Modes of seafloor generation at a melt-poor ultraslow-spreading ridge
Mathilde Cannat;Daniel Sauter;Véronique Mendel;Etienne Ruellan.
Geology (2006)
Strength of slightly serpentinized peridotites: Implications for the tectonics of oceanic lithosphere
J. Escartín;G. Hirth;B. Evans.
Geology (2001)
Constraints on deformation conditions and the origin of oceanic detachments: The Mid‐Atlantic Ridge core complex at 15°45′N
J. Escartin;C. Mevel;Christopher John MacLeod;A. M. McCaig.
Geochemistry Geophysics Geosystems (2003)
Widespread active detachment faulting and core complex formation near 13° N on the Mid-Atlantic Ridge
Deborah K. Smith;Johnson R. Cann;Javier E. Escartin.
Nature (2006)
Discovery of a magma chamber and faults beneath a Mid-Atlantic Ridge hydrothermal field
Satish C. Singh;Wayne C. Crawford;Hélène Carton;Tim Seher.
Nature (2006)
Effects of serpentinization on the lithospheric strength and the style of normal faulting at slow-spreading ridges
J. Escartín;G. Hirth;B. Evans.
Earth and Planetary Science Letters (1997)
Fault rotation and core complex formation : significant processes in seafloor formation at slow-spreading mid-ocean ridges (Mid-Atlantic Ridge, 13°–15°N)
Deborah K. Smith;Javier E. Escartin;Hans A. Schouten;Johnson R. Cann.
Geochemistry Geophysics Geosystems (2008)
Mid-Atlantic Ridge–Azores hotspot interactions: along-axis migration of a hotspot-derived event of enhanced magmatism 10 to 4 Ma ago
Mathilde Cannat;Anne Briais;Christine Deplus;Javier Escartı́n;Javier Escartı́n.
Earth and Planetary Science Letters (1999)
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