Strength of the geomagnetic field in the Cretaceous Normal Superchron: New data from submarine basaltic glass of the Troodos Ophiolite

By Lisa Tauxe, H. Staudigel. 2004

344 citations recorded by the source corpus.

Subfields: Atmospheric Science, Geophysics, Molecular Biology

View Paper: https://www.semanticscholar.org/paper/005e959e8a42967afc7a5ec2767fdfd9c9f3cabc

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. G. Hulot
2. Catherine Constable
3. Nils Olsen
4. Mioara Mandea
5. A. Biggin
6. Cor G. Langereis
7. Christopher C. Finlay
8. Geert H. M. A. Strik

In Geophysics

1. G. Hulot
2. Catherine Constable
3. Mioara Mandea
4. Christopher C. Finlay
5. A. Biggin
6. Nils Olsen
7. Cor G. Langereis
8. Geert H. M. A. Strik

In Molecular Biology

1. G. Hulot
2. Mioara Mandea
3. Catherine Constable
4. Nils Olsen
5. Christopher C. Finlay
6. A. Biggin
7. Cor G. Langereis
8. Geert H. M. A. Strik

Citations in the corpus

• Reliable absolute palaeointensities independent of magnetic domain state (2006, methodology): “Various versions of the Thellier technique have been developed to detect alteration and multidomain behaviour involving zero-field heatings followed by in-field heatings for each temperature step [13], the inverted sequence per temperature step [14], or alternating the zero-field and in-field steps ”
• Source of oceanic magnetic anomalies and the geomagnetic polarity time scale (2007, result): “intensity during the KQZ may have been high (Tarduno et al., 2001; Tauxe and Staudigel, 2004), especially compared to the JQZ, whose low-amplitude anomalies might be indicative of low average field intensity in the Jurassic (McElhinny and Larson, 2003; Prévot et al.”
• The Magnetic Field of Planet Earth (2010, background): “Submarine basaltic glasses have also been confirmed as good candidates for paleointensity work (Pick and Tauxe 1993; Carlut and Kent 2000; Tauxe and Staudigel 2004) despite some criticism (e.g. Heller et al. 2002).”
• The paleomagnetism of single silicate crystals: Recording geomagnetic field strength during mixed polarity intervals, superchrons, and inner core growth (2006, background): “Nevertheless, these are of very high technical quality, and some high paleointensity values are seen in the individual sample results for the Cretaceous Normal Polarity Superchron [Tauxe and Staudigel, 2004].”
• Toward an optimal geomagnetic field intensity determination technique (2004, methodology): “[42] Tauxe and Staudigel [2004] propose a new paleointensity protocol by combining the Aitken (In-field, Zero-field; IZ), and Coe (Zero-field, Infield; ZI), and pTRM tail check methods (called the IZZI method).”
• The intensity of the geomagnetic field in the late-Archaean: new measurements and an analysis of the updated IAGA palaeointensity database (2009, methodology): “Those points which were produced by IZ double heating steps (in which the remagnetisation were performed before the demagnetisation; Tauxe and Staudigel, 2004) are expected to be far more affected by the imparting of CRM than points produced by ZI points.”