Results 221 to 230 of about 66,103 (324)
Abstract Several geological and geophysical studies suggest the small‐scale presence of low viscosity zone (i.e., LVZ) beneath the Quaternary volcanoes of northeastern Japan. Before the 2011 Mw9.0 Tohoku‐oki earthquake, scientists hypothesized that these LVZs cause localized crustal deformations around the Quaternary volcanoes. However, the deformation‐
Sambuddha Dhar+2 more
wiley +1 more source
Diverse and highly differentiated lava suite in Jezero crater, Mars: Constraints on intracrustal magmatism revealed by Mars 2020 PIXL. [PDF]
Schmidt ME+32 more
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Gravity and Magnetic Field Signatures in Hydrothermally Affected Regions on Mars
Abstract Multiple lines of evidence indicate that liquid water‐rock interactions occurred on ancient Mars, particularly within the crust, where hydrothermal systems have been hypothesized. Such hydrothermal circulation (HC) can significantly lower temperatures in the crust, thereby restricting the viscoelastic relaxation of impact craters. Craters with
Anna Mittelholz+3 more
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Inference of a plume conduit beneath the Réunion Island from 3D migration of Ps conversions from the mantle transition zone. [PDF]
Rao BP, Kumar MR.
europepmc +1 more source
Textures and olivine fabrics of the horoman ultramafic rocks, Japan.
Kiyoaki Niida
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Abstract The essentially non‐magmatic continental rift system of the Upper Rhine Graben (URG) is segmented and characterized by intra‐rift sub‐basins that exhibit NE to NW trends suggesting complex basin development during rifting. Structural modeling and analyses of an about 40 km2 3D seismic survey from the northern part of the central URG segment ...
Florian Bauer+4 more
wiley +1 more source
A high-resolution in situ X-ray diffraction study of mineral transitions due to post-hydration heating in CM chondrite meteorites. [PDF]
Jenkins LE+8 more
europepmc +1 more source
Strength and water weakening of mantle minerals, olivine, wadsleyite and ringwoodite [PDF]
Jiuhua Chen+4 more
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Abstract Interactions between mantle plumes and mid‐ocean ridges create considerable spatial variation in composition along ridge axes. What is less well known is the temporal variation in MORB compositions along single mantle flow lines. IODP Expeditions 390/393/390C/395E recovered basaltic basement from seven sites along a flow line, the South ...
P. D. Kempton+9 more
wiley +1 more source