Literature DB >> 17750890

Geomagnetic reversal in brunhes normal polarity epoch.

J D Smith, J H Foster.   

Abstract

The magnetic stratigraphly of seven cores of deep-sea sediment established the existence of a short interval of reversed polarity in the upper part of the Brunches epoch of normal polarity. The reversed zone in the cores correlates well with paleontological boundaries and is named the Blake event. Its boundaries are estimated to be 108,000 and 114,000 years ago +/- 10 percent.

Entities:  

Year:  1969        PMID： 17750890     DOI： 10.1126/science.163.3867.565

Source DB:  PubMed          Journal:  Science        ISSN： 0036-8075            Impact factor:   47.728


  2 in total

1.  Authigenic 10Be/9Be ratio signatures of the cosmogenic nuclide production linked to geomagnetic dipole moment variation since the Brunhes/Matuyama boundary.

Authors:  Quentin Simon; Nicolas Thouveny; Didier L Bourlès; Jean-Pierre Valet; Franck Bassinot; Lucie Ménabréaz; Valéry Guillou; Sandrine Choy; Luc Beaufort
Journal:  J Geophys Res Solid Earth       Date:  2016-11-14       Impact factor: 3.848

2.  Direct terrestrial-marine correlation demonstrates surprisingly late onset of the last interglacial in central Europe.

Authors:  Mark J Sier; Wil Roebroeks; Corrie C Bakels; Mark J Dekkers; Enrico Brühl; Dimitri De Loecker; Sabine Gaudzinski-Windheuser; Norbert Hesse; Adam Jagich; Lutz Kindler; Wim J Kuijper; Thomas Laurat; Herman J Mücher; Kirsty E H Penkman; Daniel Richter; Douwe J J van Hinsbergen
Journal:  Quat Res       Date:  2011-01       Impact factor: 2.720
  2 in total

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