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pro vyhledávání: '"Jon Kirby"'
Autor:
Jon Kirby
A common method used to evaluate dynamic topography amplitudes begins with an estimate of Moho depth, usually from seismic data but sometimes - or also - from the inversion of gravity data. Then the principles of Airy isostasy are applied: surface to
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b8788a6a7213fbaf296d052a54e18f04
https://doi.org/10.5194/egusphere-egu2020-2132
https://doi.org/10.5194/egusphere-egu2020-2132
Publikováno v:
Geophysical Journal International. 214:623-634
Lithospheric effective elastic thickness (T-e), a proxy for plIate strength, is helpful for the understanding of subduction characteristics. Affected by curvature, faulting and magma activity, lithospheric strength near trenches should be weakened bu
Publikováno v:
Journal of Geodesy. 92:149-168
We describe the computation of the first Australian quasigeoid model to include error estimates as a function of location that have been propagated from uncertainties in the EGM2008 global model, land and altimeter-derived gravity anomalies and terra
Publikováno v:
GEOPHYSICS. 82:G71-G76
We have identified a gap in the literature on error propagation in the gravimetric terrain correction. Therefore, we have derived a mathematical framework to model the propagation of spatially correlated digital elevation model errors into gravimetri
Publikováno v:
Gondwana Research. 42:49-62
As a proxy for long-term lithospheric strength, detailed information on lateral effective elastic thickness (Te) variations can aid in understanding the distribution pattern of surface deformation and its response to long-term forces. Here we present
Autor:
Jon Kirby
Publikováno v:
Geophysical Journal International.
Publikováno v:
Earth and planetary science letters, 2015, Vol.419, pp.43-51 [Peer Reviewed Journal]
Lithospheric strength variations both influence and are influenced by many tectonic processes, including orogenesis and rifting cycles. The long, complex, and highly anisotropic histories of the continental lithosphere might lead to a natural expecta
Publikováno v:
Journal of Geodynamics. 81:30-40
The effective elastic thickness, Te, has been calculated in the collision zone between Arabia and Eurasia in Iran from the wavelet coherence. The wavelet coherence is calculated from Bouguer anomalies and topography data using the isotropic fan wavel
Autor:
Jon Kirby
Publikováno v:
Tectonophysics. 631:87-116
The effective elastic thickness ( T e ) is a geometric measure of the flexural rigidity of the lithosphere, which describes the resistance to bending under the application of applied, vertical loads. As such, it is likely that its magnitude has a maj
Autor:
Jon Kirby, Christopher J. Swain
Publikováno v:
Geophysical Journal International. 199:391-401
SUMMARY Recent studies have inferred patterns of rheological weakness in the lithosphere from analyses of the coherence between gravity and topography data, and related these to tectonic evolution andlithosphericrheology.Themethodsemployedallattemptt