Upper-plate magma-poor rifted margins: Stratigraphic architecture and structural evolution

Isabelle Haupert, Gianreto Manatschal, Alessandro Decarlis, Patrick Unternehr

Research output: Contribution to journalArticlepeer-review

77 Scopus citations

Abstract

Although it is generally accepted that many distal, magma-poor rifted margins are asymmetric and can be divided into lower and upper plate margins, little is known about the details of how and when this asymmetry evolves and how upper and lower plate margins can be distinguished. This is due to the fact that most papers focused on the so called lower plate margins, while the upper plate margins remained less well understood, mainly due to the lack of public accessible drill hole data. The aim of this paper is to provide a first order description of the global architecture and stratigraphic evolution of an upper plate, magma-poor rifted margin. In order to provide such a template, we focused on 2 seismic sections, the ION-1000 line (East Indian margin), and the SCREECH 2 line (Newfoundland margin) and describe key, km-scale outcrops from the fossil European margin exposed in the Western/Central Alps, all of which document classical upper plate margins. Based on these data we show that upper plate magma-poor rifted margins can be characterized by a staircase type architecture with terraces (T1, T2, T3) and ramps (R1, R2) that result as a consequence of an evolution through a coupling, exhumation and breakup stage. 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. From these observations we develop a conceptual model for the evolution of upper-plate margins and discuss the applicability of this model for different strain rates, rates of subsidence and sedimentation rates.

Original languageBritish English
Pages (from-to)241-261
Number of pages21
JournalMarine and Petroleum Geology
Volume69
DOIs
StatePublished - 1 Jan 2016

Keywords

  • Crustal architecture
  • Hyper-extension
  • Ocean-continent transition
  • Tectono-stratigraphic evolution
  • Upper plate magma-poor rifted margins

Fingerprint

Dive into the research topics of 'Upper-plate magma-poor rifted margins: Stratigraphic architecture and structural evolution'. Together they form a unique fingerprint.

Cite this