Zobrazeno 1 - 10
of 18
pro vyhledávání: '"Yu. Podladchikov"'
Publikováno v:
Izvestiya, Physics of the Solid Earth. 43:67-74
The paper is devoted to the modeling of processes of inelastic nonhydrostatic compaction and decompaction of low porosity geomaterials such that each pore can be considered as an isolated cavity in a solid matrix. A real material containing a large n
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7ce89e6e3eb3a4635b71901e5c9c5314
https://doi.org/10.1134/s1069351307010077
https://doi.org/10.1134/s1069351307010077
Autor:
Yu. Yu. Podladchikov, Daniel W. Schmid
Publikováno v:
Philosophical Magazine. 86:3409-3423
A combination of thin- and thick-plate theories, and finite element models is used to systematically analyze folding in multilayer stacks. We show that if the interlayer spacing is large, individual layers fold as single layers, if the spacing is sma
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::979fca122d909a27b690d96c28990e5f
https://doi.org/10.1080/14786430500380175
https://doi.org/10.1080/14786430500380175
Publikováno v:
Terra Nova. 13:354-359
The lithosphere is subject to fluctuations in temperature and pressure during the formation of sedimentary basins. These fluctuations cause metamorphic reactions that change the density of the lithosphere, which, in turn, influences basin subsidence.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2d88ae93d15659787555bf1927c69332
https://doi.org/10.1046/j.1365-3121.2001.00371.x
https://doi.org/10.1046/j.1365-3121.2001.00371.x
Publikováno v:
Tectonophysics. 324:137-168
The near-surface compaction regime of most sedimentary basins is characterized by hydrostatic fluid pressures and is therefore determined entirely by sediment matrix rheology. Within this regime, compaction is initially well described by a pseudoelas
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3a93eedd6a3d44bcdfb5b4ad4a028c9e
https://doi.org/10.1016/s0040-1951(00)00084-6
https://doi.org/10.1016/s0040-1951(00)00084-6
Publikováno v:
Visual Geosciences. 4:1-15
We analyzed and compared the mixing properties of 2-D mantle convection models. Two rheologically different models, Newtonian and non-Newtonian (power-law), were considered with both the line and field methods. The line method is based on monitoring
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f62ea31f11b72991e06743db50a1cc6b
https://doi.org/10.1007/s10069-999-0001-y
https://doi.org/10.1007/s10069-999-0001-y
Publikováno v:
Geodinamica Acta. 11:55-84
Compaction driven fluid flow is inherently unstable such that an obstruction to upward fluid flow (i.e. a shock) may induce fluid-filled waves of porosity, propagated by dilational deformation due to an effective pressure gradient within the wave. Vi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8e3f30830654a42de0f0257984ed2d44
https://doi.org/10.1080/09853111.1998.11105311
https://doi.org/10.1080/09853111.1998.11105311
Autor:
Yu. Podladchikov, F.J.G. (Frank) van den Belt, A.P. Samoyluk, P.L. de Boer, N.Ya. Zaykovsky, E.S. Dvorjanin, M.G. Egurnova
Publikováno v:
Tectonophysics. 268:169-187
An integrated approach combining the available geological-geophysical information was employed to construct a series of paleogeographic maps of the northwestern part of the Dnieper Donets Basin (DDB) during the Late Visean-Serpukhovian (Early Carboni
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::19a501a085d973433dd8d40d6b37d85a
https://doi.org/10.1016/s0040-1951(96)00235-1
https://doi.org/10.1016/s0040-1951(96)00235-1
Publikováno v:
Tectonophysics. 228:199-210
We have studied the initiation of salt diapirs with frictional overburdens under lateral compression and extension. The overburden is assumed to be elasto-plastic with Mohr-Coulomb yield criterion and non-associated flow rule. Plastic flow localizes
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::53b3781d6fb7791c15aabdda4138922a
https://doi.org/10.1016/0040-1951(93)90341-g
https://doi.org/10.1016/0040-1951(93)90341-g
Publikováno v:
Tectonophysics. 228:189-198
Numerically modelled diapirs that rise into overburdens with viscous rheology produce a large variety of shapes. This work uses the finite-element method to study the development of diapirs that rise towards a surface on which a diapir-induced topogr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e2bc3616abbffc668707417126bea867
https://doi.org/10.1016/0040-1951(93)90340-p
https://doi.org/10.1016/0040-1951(93)90340-p
Autor:
Yu. Yu. Podladchikov, B.A. Litvinovsky
Publikováno v:
Lithos. 30:93-107
Many data show that large masses of silicic magma can be formed by crustal anatexis under the influence of volatiles, possibly enriched in primary water derived from a mantle source. In the present paper, a model of crustal anatexis, accompanied by a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fb219d70c556a0a857dade7addcc6603
https://doi.org/10.1016/0024-4937(93)90009-2
https://doi.org/10.1016/0024-4937(93)90009-2