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- W3155800275 abstract "Rifted margins are the result of the successful process of thinning and breakup of the continental lithosphere leading to the formation of new oceanic lithosphere. Observations on rifted margins are now integrating an increasing amount of multi-channel seismic data and drilling of several Continent-Ocean Transitions. Based on large scale geometries and domains observed on high-quality multi-channel seismic data, this article proposes a classification reflecting the mechanical behavior of the crust from localized to diffuse deformation (strong/coupled to weak/decoupled mechanical behaviors) and magmatic intensity leading to breakup from magma-rich to magma-poor margins. We illustrate a simple classification based on mechanical behavior and magmatic production with examples of rifted margins. We propose a non-exhaustive list of forcing parameters that can control the initial rifting conditions but also their evolution through time. Therefore, rifted margins are not divided into opposing types, but described as a combination and continuum that can evolve through time and space." @default.
- W3155800275 created "2021-04-26" @default.
- W3155800275 creator A5036338512 @default.
- W3155800275 creator A5038864948 @default.
- W3155800275 creator A5040502223 @default.
- W3155800275 date "2021-04-14" @default.
- W3155800275 modified "2023-10-14" @default.
- W3155800275 title "Rifted margins classification and forcing parameters" @default.
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