Results 231 to 240 of about 627,703 (284)

Depositional and Hydrological Relationships Between Buried Dead Ice and the Active Layer in the McMurdo Dry Valleys, Antarctica: A Study of Sediment Geochemistry and Cation Concentrations

open access: yesPermafrost and Periglacial Processes, EarlyView.
ABSTRACT The McMurdo Dry Valleys, the largest ice‐free region in Antarctica, are home to a cold‐desert hydrologic system of glaciers, snowbanks, streams, and lakes. Freshwater is also stored as dead glacial ice, which is poorly constrained in terms of ion concentrations and interactions with both in situ and overlying sediments.
Matthew C. Witscheber, Kate M. Swanger
wiley   +1 more source

Structural barriers control the spatial extent of slow earthquake slip. [PDF]

open access: yesNat Commun
Akuhara T   +18 more
europepmc   +1 more source

Unveiling the clinical and proteomic spectrum of relapsing polychondritis with respiratory involvement. [PDF]

open access: yesFront Immunol
Fang X   +14 more
europepmc   +1 more source

Orientation-Dependent Reinforcing Mechanisms of SiC/Carbon Nanotube Composites: A Reactive Molecular Dynamics Simulation Study. [PDF]

open access: yesLangmuir
Su Y   +9 more
europepmc   +1 more source

A unique electrical resistivity experiment reveals the 3D interior of Piton de la Fournaise. [PDF]

open access: yesSci Rep
Gailler L   +7 more
europepmc   +1 more source

Monitoring of Volcano deformation

open access: yes, 2022
Monitoring ground surface deformation is an essential component of volcano monitoring, along with other techniques, such as seismology, geochemistry and geology. This chapter presents the different sources at the origin of the deformation observed in a volcanic context, followed by a review of the various techniques used for measuring such deformation.
Cayol, Valérie   +3 more
openaire   +3 more sources
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Deformed symmetrical volcanoes

Geology, 2005
Analog modeling of volcanic cones traversed by strike-slip faulting was conducted, and the cones were analyzed for deformation characteristics. The study shows that symmetrical volcanoes that have undergone basal strike-slip offset may be deformed internally without manifesting any change in their conical shape.
G. Norini, A.M.F. Lagmay
openaire   +1 more source

The role of basement in volcano deformation

Geological Society, London, Special Publications, 1996
AbstractGrowing volcanoes load their basements, causing isostatic flexure, compaction and brittle and ductile deformation. Deformation of basement in turn exerts stress onto the edifice, which also responds by deforming. This deformation will be gradual or catastrophic, depending on the nature of the cone, and the properties of the underlying rocks ...
Benjamin Van Wyk De Vries, Andrea Borgia
openaire   +1 more source

Understanding stress and deformation in active volcanoes

Tectonophysics, 2009
No eruption, no caldera collapse, and no large landslide can takeplaceinavolcanounlessitsstateofstressissuitablefortheassociatedtype of rock failure. The state of stress, in turn, results in deformation,andbothstressanddeformationdependonthemechanicalpropertiesof the rocks that constitute the volcano. Understanding stress anddeformation in volcanoes is
GUDMUNDSSON A   +2 more
openaire   +3 more sources

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