FN Archimer Export Format
PT J
TI The Mid‐Atlantic Ridge Near 13°20′N: High‐Resolution Magnetic and Bathymetry Imaging
BT 
AF SEARLE, R. C.
   MACLEOD, C. J.
   PEIRCE, C.
   RESTON, T. J.
AS 1:1;2:2;3:1;4:3;
FF 1:;2:;3:;4:;
C1 Univ Durham, Dept Earth Sci, Durham, England.
   Cardiff Univ, Sch Earth & Ocean Sci, Cardiff, S Glam, Wales.
   Univ Birmingham, Sch Geog Earth & Environm Sci, Birmingham, W Midlands, England.
C2 UNIV DURHAM, UK
   UNIV CARDIFF, UK
   UNIV BIRMINGHAM, UK
IF 2.623
TC 14
UR https://archimer.ifremer.fr/doc/00499/61031/64436.pdf
   https://archimer.ifremer.fr/doc/00499/61031/64437.pdf
LA English
DT Article
CR ODEMAR
BO Pourquoi pas ?
DE ;mid-ocean ridges;oceanic core complexes;magnetic anomalies;microtopography
AB We describe detailed magnetic and bathymetric studies around 13 degrees N on the Mid-Atlantic Ridge, a site of extensive detachment faulting. Inversion of closely spaced sea surface magnetic anomalies reveals a disorganized pattern of magnetization, with anomalies younger than anomaly 2 being poorly delineated. The Brunhes anomaly width is highly variable but averages similar to 60% of that predicted for the regional spreading rate. It is often split, both along and across axis, by apparently reversely magnetized crust. Gaps in the Brunhes anomaly match gaps in the neovolcanic zone inferred from acoustic backscatter. A strong negative magnetization is associated with the oceanic core complex (OCC) at 13 degrees 2'N (OCC1320) and is inferred to arise from exhumed old, reversely magnetized lithosphere. The inferred position of the magmatic axis implies similar to 30% asymmetry of crustal accretion post-anomaly-2. Higher spatial resolution magnetic anomalies near the seafloor, measured by autonomous underwater vehicle, are qualitatively similar to earlier deep-towed data but differ somewhat from the sea surface magnetics. We interpret this mismatch as reflecting the differing sensitivities of the two observing geometries and the existence of a highly heterogeneous topography and magnetization. This suggests that a strongly three-dimensional structure exists, more compatible with a geodynamic model where neighboring OCCs are not connected but evolve independently. A modeled near-seafloor profile through OCC1320 shows low positive magnetization below the smooth dome. A second profile, running E-W between two OCCs, shows high magnetization coinciding with a large seamount, reflecting recent off-axis volcanism. Measured microbathymetry reveals extensive small volcanic cones on this seamount and confirms previous interpretations of OCC morphology. 
PY 2019
PD JAN
SO Geochemistry Geophysics Geosystems
SN 1525-2027
PU Amer Geophysical Union
VL 20
IS 1
UT 000458607200015
BP 295
EP 313
DI 10.1029/2018GC007940
ID 61031
ER

EF