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Rifted margins classification and forcing parameters.

F Sapin1, J-C Ringenbach2, C Clerc3

  • 1Total S.A., CSTJF, Avenue Larribau, Pau, France. francois.sapin@total.com.

Scientific Reports
|April 15, 2021
PubMed
Summary
This summary is machine-generated.

This study classifies rifted margins based on crustal mechanical behavior and magmatic intensity, revealing a continuum of deformation rather than distinct types. Understanding these factors is key to comprehending continental breakup and the formation of oceanic lithosphere.

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Area of Science:

  • Geology
  • Geophysics
  • Tectonics

Background:

  • Rifted margins form from continental lithosphere thinning and breakup, creating new oceanic lithosphere.
  • Multi-channel seismic data and drilling are crucial for studying Continent-Ocean Transitions.
  • Existing classifications often present opposing types of rifted margins.

Purpose of the Study:

  • To propose a new classification system for rifted margins.
  • To reflect the mechanical behavior of the crust (localized to diffuse deformation).
  • To incorporate magmatic intensity (magma-rich to magma-poor) in the classification.

Main Methods:

  • Analysis of large-scale geometries and domains from high-quality multi-channel seismic data.
  • Integration of drilling data from Continent-Ocean Transitions.
  • Development of a classification based on crustal mechanical behavior and magmatic production.

Main Results:

  • A classification framework is proposed based on coupled (strong) to decoupled (weak) mechanical behaviors.
  • The classification considers the spectrum from magma-rich to magma-poor margins.
  • Examples illustrate the proposed classification of rifted margins.

Conclusions:

  • Rifted margins represent a continuum of deformation and magmatic styles, not discrete opposing types.
  • The classification highlights the interplay between mechanical behavior and magmatic production.
  • Forcing parameters influencing rifting evolution are identified, emphasizing temporal and spatial variability.