Causes of oceanic crustal thickness oscillations along a 74-M Mid-Atlantic ridge flow line
Shinevar, William J.
Mark, Hannah F.
Codillo, Emmanuel A.
Brown, Stephanie M.
Smalls, Paris T.
Le Roux, Véronique
Behn, Mark D.
MetadataShow full item record
Keywordocean crustal thickness; faulting style; Mid‐Atlantic Ridge; spectral analysis; oceanic core complex; magma input variation
Gravity, magnetic, and bathymetry data collected along a continuous 1,400‐km‐long spreading‐parallel flow line across the Mid‐Atlantic Ridge indicate significant tectonic and magmatic fluctuations in the formation of oceanic crust over a range of time scales. The transect spans from 28 Ma on the African Plate to 74 Ma on the North American plate, crossing the Mid‐Atlantic Ridge at 35.8°N. Gravity‐derived crustal thicknesses vary from 3–9 km with a standard deviation of 1.0 km. Spectral analysis of bathymetry and residual mantle Bouguer anomaly show a diffuse power at >1 Myr and concurrent peaks at 390, 550, and 950 kyr. Large‐scale (>10 km) mantle thermal and compositional heterogeneities, variations in upper mantle flow, and detachment faulting likely generate the >1 Myr diffuse power. The 550‐ and 950‐kyr peaks may reflect the presence of magma solitons and/or regularly spaced ~7.7 and 13.3 km short‐wavelength mantle compositional heterogeneities. The 390‐kyr spectral peak corresponds to the characteristic spacing of faults along the flow line. Fault spacing also varies over longer periods (>10 Myr), which we interpret as reflecting long‐lived changes in the fraction of tectonically versus magmatically accommodated extensional strain. A newly discovered off‐axis oceanic core complex (Kafka Dome) found at 8 Ma on the African plate further suggests extended time periods of tectonically‐dominated plate separation. Fault spacing negatively correlates with gravity‐derived crustal thickness, supporting a strong link between magma input and fault style at mid‐ocean ridges.
Author Posting. © American Geophysical Union, 2019. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geochemistry, Geophysics, Geosystems 20, (2019): 6123-6139, doi: 10.1029/2019GC008711.
Suggested CitationShinevar, W. J., Mark, H. F., Clerc, F., Codillo, E. A., Gong, J., Olive, J., Brown, S. M., Smalls, P. T., Liao, Y., Le Roux, V., & Behn, M. D. (2019). Causes of oceanic crustal thickness oscillations along a 74-M Mid-Atlantic Ridge flow line. Geochemistry Geophysics Geosystems, 20, 6123-6139.
Showing items related by title, author, creator and subject.
Shinevar, William J.; Mark, Hannah F.; Clerc, Fiona; Codillo, Emmanuel A.; Gong, Jianhua; Olive, Jean-Arthur; Brown, Stephanie M.; Smalls, Paris T.; Liao, Yang; Le Roux, Véronique; Behn, Mark D. (2019-11-12)Gravity, magnetic, and bathymetry data collected along a continuous 1400-km-long spreading-parallel flow line across the Mid-Atlantic Ridge indicate significant tectonic and magmatic fluctuations in the formation of oceanic ...
Quantitative analysis of abyssal hills in the Atlantic Ocean : a correlation between inferred crustal thickness and extensional faulting Goff, John A.; Tucholke, Brian E.; Lin, Jian; Jaroslow, Gary E.; Kleinrock, Martin C. (American Geophysical Union, 1995-11-10)A recent cruise to the Office of Naval Research Atlantic Natural Laboratory obtained ∼100% Hydrosweep bathymetrie coverage, >200% Hawaii MRl (HMRl) side scan coverage, gravity and magnetics over an area spanning three ridge ...
Wang, Tingting; Lin, Jian; Tucholke, Brian E.; Chen, Yongshun J. (American Geophysical Union and the Geochemical Society, 2011-03-31)Gravity-derived crustal thickness models were calculated for the North Atlantic Ocean between 76°N and the Chain Fracture Zone and calibrated using seismically determined crustal thickness. About 7% of the ocean crust is ...