Sentence examples for evolution of the margin from inspiring English sources

In this paper we report the U Pb and Hf isotopes of detrital zircons from the Late Carboniferous bauxite layer and use these data to constrain the tectonic evolution of the margin of the NCC.

We also defined key stratigraphic levels that we try to link with the evolution of the margin which enables us to link the tectonic evolution with the creation of accommodation space and formation of the staircase architecture that characterizes the upper plate margin.

The interpretation of a seismic grid using seismic and sequence stratigraphy and structural geology approaches in a dedicated GIS environment led to the generation of 2-D models of relevant geological surfaces, isochron maps, a 3-D digital model of the subsurface and to the reconstruction of the geological evolution of the margin with a resolution of 100 ka.

The Mount Painter Province was located near the margin of both the South Australian Craton and the North Australian Craton, which allows comparisons of the tectonic evolution of these margins and provides context for the evolution of the eastern Proterozoic Australia for both the Columbia and Gondwana supercontinents.

We present a 3D conceptual model for the evolution of the western margin of the Levant Basin.

The response of bedrock channels to differential rock uplift in eastern Qilian Mountain significantly dictates the topographic evolution of the northeastern margin of the Tibetan Plateau.

The subduction of the floor of the Pacific Ocean dominated the evolution of the Pacific margin of Asia, especially during the second half of the Mesozoic Era.

The late-Quaternary evolution of the continental margin took place under the influence of an asymmetric relative fourth-order sea-level cycle punctuated by higher frequency cycles.

In this dissertation, I develop and apply basement and detrital K-feldspar coupled 40Ar/39Ar and Pb isotopic analysis to evaluate the Late Cretaceous/Cenozoic evolution of the California margin.

We suggest that structural and igneous evolution of the Korean margin, although it is in a back-arc setting, can be explained by the processes occurring at the passive continental margin with magmatism influenced by asthenospheric upwelling.

From these results, we suggest that the post-rift evolution of the Namibian margin was associated, during the Upper Cretaceous, to the rejuvenation of its continental relief triggered by a climate change during the Turonian and by a slow long-term rock-uplift during the Cenozoic.