An inverse method for determining lithospheric strain rate variation on geological timescales
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Extricating dynamic topography from subsidence patterns: Examples from Eastern North America's passive margin
2020, Earth and Planetary Science LettersSubsidence transition during the post-rift stage of the Dongpu Sag, Bohai Bay Basin, NE China: A new geodynamic model
2018, Journal of Asian Earth SciencesNeogene residual subsidence and its response to a sinking slab in the deep mantle of eastern China
2017, Journal of Asian Earth SciencesCitation Excerpt :To extract the residual subsidence, we compared theoretical results with the observed post-rift tectonic subsidence. The back-stripping technique was used to calculate the observed tectonic subsidence, and a 1D strain rate inversion model was used to calculate the theoretical tectonic subsidence (Li and Liu, 2015; McKenzie, 1978; Song et al., 2010; White, 1993, 1994) (Fig. 3). The back-stripping technique, which is based on the method of Sclater and Christie (1980), was used to calculate the observed tectonic subsidence.
The initiation and tectonic regimes of the Cenozoic extension in the Bohai Bay Basin, North China revealed by numerical modelling
2017, Journal of Asian Earth SciencesCitation Excerpt :When the total strength of the lithosphere (S) is equal to this tectonic force, the extension will start (Yamasaki and Stephenson, 2009, 2011). In order to get the strain rate, the inversed numerical method from White (1994) is applied, which varies the strain rate (G(t)) each time until the difference between the calculated and the observed subsidences is minimized. The observed and calculated subsidences are illustrated in Fig. 9.