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pro vyhledávání: '"Lawrence Hongliang Wang"'
Two-phase flow equations that couple solid deformation and fluid migration have opened new research trends in geodynamical simulations and modeling of subsurface engineering operations. A numerical model based on two-phase flow equations has been use
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8e90c261ac12746d017f3b5af3bb40ed
https://doi.org/10.5194/egusphere-egu23-17169
https://doi.org/10.5194/egusphere-egu23-17169
Autor:
G. J. Irvine, Bruce A. Kjarsgaard, D. Graham Pearson, John Armstrong, Jingao Liu, Andrew J. Schaeffer, Lawrence Hongliang Wang, Kathy A. Mather, Maya G. Kopylova
Publikováno v:
Nature. 592:732-736
Cratons are Earth’s ancient continental land masses that remain stable for billions of years. The mantle roots of cratons are renowned as being long-lived, stable features of Earth’s continents, but there is also evidence of their disruption in t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b6cb1a6f1bb17414a2498fb421ac9092
https://doi.org/10.1038/s41586-021-03395-5
https://doi.org/10.1038/s41586-021-03395-5
Two-phase flow equations that couple solid deformation and fluid migration have opened new research trends in geodynamical simulations and modelling of subsurface engineering operations. The physical nonlinearity of fluid-rock systems and strong coup
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bd43c045631e6543849b210c64cd2aba
https://doi.org/10.5194/egusphere-egu22-8033
https://doi.org/10.5194/egusphere-egu22-8033
Autor:
Jingao Liu, D Pearson, Lawrence Hongliang Wang, Kathy Mather, Bruce Kjarsgaard, Andrew Schaeffer, Maya Kopylova, Gordon Irvine, John Armstrong
Publikováno v:
Goldschmidt2022 abstracts.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ee89b6fa16f5f01407c7f269ac16371e
https://doi.org/10.46427/gold2022.11982
https://doi.org/10.46427/gold2022.11982
Autor:
Lawrence Hongliang Wang, James M. Scott, Peter B. Kelemen, Jeroen van Hunen, Kristoffer Szilas, Thomas Chacko, D. Graham Pearson, Jingao Liu, Andrew J. Schaeffer
Publikováno v:
Pearson, D G, Scott, J M, Liu, J, Schaeffer, A, Wang, L H, Hunen, J V, Szilas, K, Chacko, T & Kelemen, P B 2021, ' Deep continental roots and cratons ', Nature, vol. 596, pp. 199-210 . https://doi.org/10.1038/s41586-021-03600-5
Nature, 2021, Vol.596(7871), pp.199-210 [Peer Reviewed Journal]
Nature, 2021, Vol.596(7871), pp.199-210 [Peer Reviewed Journal]
The formation and preservation of cratons—the oldest parts of the continents, comprising over 60 per cent of the continental landmass—remains an enduring problem. Key to craton development is how and when the thick strong mantle roots that underl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::556e0eb8c404506457b2062ff0bb2851
https://curis.ku.dk/portal/da/publications/deep-continental-roots-and-cratons(1c5e85eb-878a-4ef3-b1e6-7becd76d9dad).html
https://curis.ku.dk/portal/da/publications/deep-continental-roots-and-cratons(1c5e85eb-878a-4ef3-b1e6-7becd76d9dad).html
Publikováno v:
Geophysical Journal International, vol. 229, no. 1, pp. 1-20
SUMMARY Two-phase flow equations that couple solid deformation and fluid migration have opened new research trends in geodynamic simulations and modelling of subsurface engineering. Physical non-linearity of fluid-rock systems and strong coupling bet
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7b2384c6c39c47f06f453eb23bc92efc
The coupling between fluid flow and solid deformation plays important roles in earth dynamics at different timescales and length-scales. Related processes include, magma migration and focusing in the Mid-Ocean Ridges, fluid migration after slab dehyd
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fc1da5b472e4cf8b15fef61f95568c1a
https://doi.org/10.5194/egusphere-egu21-12021
https://doi.org/10.5194/egusphere-egu21-12021
Understanding fluid flow patterns in the shallow and deep earth is one of the major challenges of modern earth sciences. Fluid flow may be slow and pervasive, or fast and focused. In the deep earth, focused fluid flow may result in, for example, dike
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0b79b7fb560e7fac62d7c2be19c8f48f
https://doi.org/10.5194/egusphere-egu21-8341
https://doi.org/10.5194/egusphere-egu21-8341
Autor:
Viktoriya M. Yarushina, Lawrence Hongliang Wang, David Connolly, Gábor Kocsis, Ingrid Fæstø, Stephane Polteau, Assia Lakhlifi
Publikováno v:
Geology
Gas chimneys, fluid-escape pipes, and diffused gas clouds are common geohazards above or below most petroleum reservoirs and in some CO2 storage sites. However, the processes driving the formation of such structures are poorly understood, as are the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::59e793db1f9f97dbdec4b021cdfc5616
https://hdl.handle.net/11250/2976700
https://hdl.handle.net/11250/2976700