scholarly journals Sea floor spreading history, I, Labrador sea, Magnetic anomalies along track

1989 ◽  
Author(s):  
W R Roest ◽  
S P Srivastava
Keyword(s):  
Magnetic Anomalies ◽  
Labrador Sea ◽  
Sea Floor ◽  
Sea Floor Spreading ◽  
Along Track

New geophysical evidence for sea-floor spreading in central Baffin Bay

1979 ◽  
Vol 16 (11) ◽  
pp. 2122-2135 ◽  
Author(s):  
H. R. Jackson ◽  
C. E. Keen ◽  
R. K. H. Falconer ◽  
K. P. Appleton
Keyword(s):  
Magnetic Anomaly ◽  
Crustal Structure ◽  
Magnetic Anomalies ◽  
Geophysical Data ◽  
Plate Motion ◽  
Labrador Sea ◽  
Sea Floor ◽  
Baffin Bay ◽  
Spreading Rates ◽  
Sea Floor Spreading

Geophysical data collected during a detailed survey in Baffin Bay have shown that lineated magnetic anomalies trending north-northwest occupy the deep central region. These anomalies exhibit maximum amplitudes of about 300 nT and can be modelled by a 1-km thick magnetic source layer divided into blocks of normal and reversed polarity. The magnetizations required are comparable with those of oceanic basalts. A striking feature of the gravity field is a 20 mGal gravity low, about 20 km wide, which runs through the centre of the bay with approximately the same trend as the magnetic lineations. The gravity low is associated with a change in crustal structure measured from seismic refraction data and sometimes with a deepening of the sediment-basement interface, reminiscent of a median valley. These results suggest that the magnetic anomalies were produced by sea-floor spreading and that the gravity low marks an extinct spreading centre in Baffin Bay. Comparisons of the magnetic anomaly profiles with a model profile computed for magnetic anomalies 13–24 (38 to 60 Ma), show good correlation between the observed and computed anomalies in the time period represented by anomalies 13–21, with slow spreading rates of about 0.3–0.4 cm yr−1 perpendicular to the spreading axis. These results are in reasonable agreement with magnetic anomaly identifications and spreading rates deduced from geophysical data in the Labrador Sea. The direction of plate motion in Baffin Bay is not well defined from the data, but the Labrador Sea data require plate motions at a highly oblique angle to the spreading centre in the bay. Peculiarities of the postulated spreading centre, including the change in crustal structure beneath the gravity low along its strike from south to north, and the decrease in coherence and amplitude of the magnetic anomalies immediately north of the survey area, may be the result of these very low spreading rates, oblique spreading and changes in spreading direction, or the proximity of this area to the junction with a possible major transform fault through the Nares Strait.

Comoros – New Evidence and Arguments for Continental Crust

2016 ◽  
Author(s):  
John Milsom ◽  
Phil Roach ◽  
Chris Toland ◽  
Don Riaroh ◽  
Chris Budden ◽  
...  
Keyword(s):  
Continental Crust ◽  
Fracture Zone ◽  
Seismic Data ◽  
Gravity Anomalies ◽  
Magnetic Anomalies ◽  
Magnetic Data ◽  
The West ◽  
Sea Floor ◽  
Inappropriate Use ◽  
Sea Floor Spreading

ABSTRACT As part of an ongoing exploration effort, approximately 4000 line-km of seismic data have recently been acquired and interpreted within the Comoros Exclusive Economic Zone (EEZ). Magnetic and gravity values were recorded along the seismic lines and have been integrated with pre-existing regional data. The combined data sets provide new constraints on the nature of the crust beneath the West Somali Basin (WSB), which was created when Africa broke away from Gondwanaland and began to move north. Despite the absence of clear sea-floor spreading magnetic anomalies or gravity anomalies defining a fracture zone pattern, the crust beneath the WSB has been generally assumed to be oceanic, based largely on regional reconstructions. However, inappropriate use of regional magnetic data has led to conclusions being drawn that are not supported by evidence. The identification of the exact location of the continent-ocean boundary (COB) is less simple than would at first sight appear and, in particular, recent studies have cast doubt on a direct correlation between the COB and the Davie Fracture Zone (DFZ). The new high-quality reflection seismic data have imaged fault patterns east of the DFZ more consistent with extended continental crust, and the accompanying gravity and magnetic surveys have shown that the crust in this area is considerably thicker than normal oceanic and that linear magnetic anomalies typical of sea-floor spreading are absent. Rifting in the basin was probably initiated in Karoo times but the generation of new oceanic crust may have been delayed until about 154 Ma, when there was a switch in extension direction from NW-SE to N-S. From then until about 120 Ma relative movement between Africa and Madagascar was accommodated by extension in the West Somali and Mozambique basins and transform motion along the DFZ that linked them. A new understanding of the WSB can be achieved by taking note of newly-emerging concepts and new data from adjacent areas. The better-studied Mozambique Basin, where comprehensive recent surveys have revealed an unexpectedly complex spreading history, may provide important analogues for some stages in WSB evolution. At the same time the importance of wide continent-ocean transition zones marked by the presence of hyper-extended continental crust has become widely recognised. We make use of these new insights in explaining the anomalous results from the southern WSB and in assessing the prospectivity of the Comoros EEZ.

Sea-floor spreading in the Labrador Sea: A new reconstruction

Geology ◽  
1989 ◽  
Vol 17 (11) ◽  
pp. 1000 ◽  
Author(s):  
W. R. Roest ◽  
S. P. Srivastava
Keyword(s):  
Labrador Sea ◽  
Sea Floor ◽  
Sea Floor Spreading

New estimates of rapid sea-floor spreading rates and the identification of young magnetic anomalies on the East Pacific rise, 6° and 11° S

1973 ◽  
Vol 19 (2) ◽  
pp. 225-229 ◽  
Author(s):  
David K. Rea ◽  
Jack Dymond ◽  
G. Ross Heath ◽  
Donald F. Heinrichs ◽  
Stephen H. Johnson ◽  
...  
Keyword(s):  
East Pacific Rise ◽  
Magnetic Anomalies ◽  
Sea Floor ◽  
East Pacific ◽  
Spreading Rates ◽  
Sea Floor Spreading

Magnetic anomalies in the Pacific and sea floor spreading

1968 ◽  
Vol 73 (6) ◽  
pp. 2069-2085 ◽  
Author(s):  
W. C. Pitman ◽  
E. M. Herron ◽  
J. R. Heirtzler
Keyword(s):  
Magnetic Anomalies ◽  
Sea Floor ◽  
The Pacific ◽  
Sea Floor Spreading
Sign in / Sign up

Export Citation Format

Share Document