Spreading rate dependence of gravity anomalies along oceanic transform faults

Nature ◽  
2007 ◽  
Vol 448 (7150) ◽  
pp. 183-187 ◽  
Author(s):  
Patricia M. Gregg ◽  
Jian Lin ◽  
Mark D. Behn ◽  
Laurent G. J. Montési

Strong magnetic anomalies associated with the axial trough of the Red Sea are considered to be related to a second phase of opening. Lack of magnetic expression of the first and wider separation is attributed to initial thinning and necking of the continental crust and, possibly, to a slow rate of spreading. The rise of the mantle during this first stage is reflected in the positive Bouguer gravity anomaly which extends over the whole Sea. A displacement of the magnetic anomaly pattern and a grouping of earthquake epicentres at latitude 19½° N delineates a transform fault. Futher offsets in the anomaly pattern between 19½° N and 23° N may be related to other transform faults presently inactive. If Sinai is treated as a separate block then the two-stage clockwise rotation of Africa to open the Red Sea leads to the southerly displacements of this block required by the geology. Negative gravity anomalies in the Gulf of Aqaba support the idea of a shear. A separate rotation of the Horn of Africa is believed to have contributed to the opening of the Gulf of Aden.


1972 ◽  
Vol 9 (8) ◽  
pp. 942-959 ◽  
Author(s):  
J. M. Woodside

Detailed maps of free-air, Bouguer, and residual gravity anomalies for a survey area 250 km wide across the Mid-Atlantic Ridge between 45° and 46 °N have been compiled. The Bouguer anomaly was terrain-corrected to a radius of 40 km. The residual anomaly was computed from the terrain-corrected Bouguer anomaly using an empirical linear relationship between the Bouguer anomaly and the bathymetry to predict a 'regional' Bouguer anomaly from the depth data. North–south and east–west trends in the gravity data are enhanced in the residual anomaly; and it is suggested that at least one short east–west transform fault may offset the ridge in a right-lateral sense. The offset is presumably a response to a change in sea-floor spreading direction from west–northwest/east–southeast to west/east about 10 m.y. ago. A change in spreading rate may have occurred at the same time. A difference in accretion rate on either side of the ridge axis is indicated by asymmetry in the gravity data and by differences in the topographic compensation across the axis. Variations in the relationship of terrain-corrected Bouguer anomaly to bathymetry within the survey area suggest that a density deficiency or buoyant forces in the upper mantle are responsible for the overall elevation of the crestal mountain region but that the topography of the high-fractured plateau may be partially compensated by undulations of the crust–mantle interface.


Nature ◽  
2004 ◽  
Vol 432 (7018) ◽  
pp. 744-747 ◽  
Author(s):  
Daniel Lizarralde ◽  
James B. Gaherty ◽  
John A. Collins ◽  
Greg Hirth ◽  
Sangmyung D. Kim

Lithosphere ◽  
2011 ◽  
Vol 3 (6) ◽  
pp. 371-378 ◽  
Author(s):  
Emilia A. Koivisto ◽  
Richard G. Gordon ◽  
Jérôme Dyment ◽  
Jafar Arkani-Hamed

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