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Contrasting stress fields on correlating margins of the South Atlantic

Salomon E, Koehn D, Passchier C, Hackspacher PC, Glasmacher UA (2015)

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Publication Status: Published

Publication Type: Journal article

Publication year: 2015

Journal

Publisher: ELSEVIER

Book Volume: 28

Pages Range: 1152-1167

Journal Issue: 3

DOI: 10.1016/j.gr.2014.09.006

Abstract

The "passiveness" of passive continental margins across the globe is currently under debate since several studies have shown that these margins may experience a variety of stress states and undergo significant vertical movement post-breakup. Of special interest is the South Atlantic, because the bounding continents have very different recent geological histories, with Africa experiencing continental rifting whereas South America is influenced by subduction on the Pacific side. It is not clear to what extent the Atlantic continental margins are subject to the same stresses and vertical motions as the main continents. To address this problem, we performed a paleostress analysis of two originally adjacent areas, i.e. NW Namibia and SE/S Brazil. Both areas are covered by the similar to 133-Ma-old Parana-Etendeka extrusives-that were emplaced shortly before or during the onset of the Atlantic rifting. Thus, the volcanics serve as a time marker for syn- or post-rift deformation. Collected fault slip data in the volcanics reveal remarkable differences between the two correlating areas. NW Namibia was dominated by extension in ENE-WSW and SW-NE directions, and by minor strike-slip movement with NW-SE directed compression. SE/S Brazil was mostly affected by strike-slip faulting, with compression oriented E-W and SW-NE. Similar fault systems appear widespread across SE Brazil and may be the combined result of flexural margin bending and the Nazca plate subduction. The results of NW Namibia differ from known compressional stress tensors in western South Africa, post-dating 90 Ma. The south-western African continental margin may thus have experienced a spatially variable stress history. Our results show that the tectonic evolution of the continental margins of the South Atlantic is not passive and that both margins vary significantly in structural style and stress fields, indicating that variable plate boundary forces play a major role in margin evolution. (C) 2014 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.

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APA:

Salomon, E., Koehn, D., Passchier, C., Hackspacher, P.C., & Glasmacher, U.A. (2015). Contrasting stress fields on correlating margins of the South Atlantic. Gondwana Research, 28(3), 1152-1167. https://doi.org/10.1016/j.gr.2014.09.006

MLA:

Salomon, Eric, et al. "Contrasting stress fields on correlating margins of the South Atlantic." Gondwana Research 28.3 (2015): 1152-1167.

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