Results 201 to 210 of about 3,746 (252)

Mercury at the Dawn of a New Exploration Phase. [PDF]

Nat Commun
Del Vecchio E, Zomerdijk-Russell S, Buoninfante S.   +2 more
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Helium isotope anomaly in groundwater prior to the 2024 Noto Peninsula earthquake. [PDF]

Nat Commun
Kagoshima T, Sano Y, Takahata N, Kawamoto Y, Shibata T, Li Y, Morishita T, Hiramatsu Y, Nakajima J.   +8 more
europepmc   +1 more source

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Crustal deformation

Reviews of Geophysics, 1995
Geodetic measurements of crustal deformation provide direct tests of geophysical models which are used to describe the dynamics of the Earth. Although geodetic observations have been made throughout history, only in the last several hundred years have they been sufficiently precise for geophysical studies. In the 19th century, these techniques included
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Migration of crustal deformation

Tectonophysics, 1979
Abstract Observations on the migration rates of crustal deformation, as recently discovered in several tectonic areas, such as the south Kanto and central Tohoku districts, Japan and the West Cordillera Mts., Peru, has opened up a new opportunity for the study of crustal dynamics.
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Models of crustal deformation

Reviews of Geophysics, 1983
This review is principally concerned with theoretical models of crustal deformation developed during this quadrennium. Observational data, as well as topics in lithospheric flexure and isostasy, are covered in companion reviews in this volume. Progress has been made toward constructing both new inelastic, and inhomogeneous elastic, models of earthquake‐
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Mechanisms of crustal deformation

Journal of the Geological Society, 1983
The energy source for crustal deformation is isotopic heating and secular cooling of the mantle. In a true solid, heat would be lost to the surface by conduction; however, solid-state creep processes allow the Earth’s solid mantle to exhibit a fluid behaviour. Thus, thermal convection can convert heating into directed motion.
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Study of crustal deformation in India

Tectonophysics, 1972
Abstract Investigations of crustal deformation at Koyna (near Poona) and Dakpathar (near Dehradun) were undertaken as a part of a research programme drawn up by the University of Roorkee. Possible applications of such studies and the general plans to be adopted for field measurements are briefly stated.
P.N. Agrawal, V.K. Gaur
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Introduction to modeling crustal deformation

Journal of Geophysical Research: Solid Earth, 1993
This special section on Modeling Crustal Deformation presents a collection of research articles prepared by several participants in the AGU Chapman Conference on Time‐Dependent Positioning. The conference was convened September 23–25, 1991, in Annapolis, Maryland.
Richard A. Snay, Sandford R. Holdahl
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Plate motions and crustal deformation

Reviews of Geophysics, 1995
Over the past 30 years, the plate tectonic paradigm has revolutionized the earth sciences through its powerful yet elegant quantitative treatment of large‐scale crustal deformation, and through its conceptually integrative role within the earth sciences.
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Crustal deformation by earthquakes and explosions

Bulletin of the Seismological Society of America, 1970
abstract Static displacements were calculated for an earth model which consists of a single layer of thickness H overlying a homogeneous half space. Localized sources simulating earthquake and explosion foci are placed at depths h=H2andh=32H.
Ari Ben-Menahem, Allon Gillon
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