FN Archimer Export Format
PT J
TI Sub-axial deformation in oceanic lower crust: Insights from seismic reflection profiles in the Enderby Basin and comparison with the Oman ophiolite
BT 
AF SAUTER, Daniel
   WERNER, Philippe
   CEULENEER, Georges
   MANATSCHAL, Gianreto
   ROSPABé, Mathieu
   TUGEND, Julie
   GILLARD, Morgane
   AUTIN, Julia
   ULRICH, Marc
AS 1:1;2:1;3:2;4:1;5:3;6:4;7:4;8:1;9:1;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;
C1 Univ Strasbourg, Inst Phys Globe Strasbourg IPGS, UMR7516 CNRS, 1 Rue Blessig, F-67084 Strasbourg, France.
   Univ Toulouse, Observ Midi Pyrenees, CNRS, Geosci Environm Toulouse GET,IRD, 14 Ave E Belin, F-31400 Toulouse, France.
   Japan Agcy Marine Earth Sci & Technol JAMSTEC, Res Inst Marine Geodynam IMG, 2-15 Natsushima, Yokosuka, Kanagawa 2370061, Japan.
   Sorbonne Univ, Inst Sci Terre Paris ISTeP, CNRS, UMR 7193, 4 Pl Jussieu, F-75005 Paris, France.
C2 UNIV STRASBOURG, FRANCE
   UNIV TOULOUSE, FRANCE
   JAMSTEC, JAPAN
   UNIV PARIS 06, FRANCE
IF 5.785
TC 11
UR https://archimer.ifremer.fr/doc/00773/88513/94286.pdf
LA English
DT Article
DE ;lower oceanic crust;oceanic accretionary processes;dipping reflectors;ocean-continent transition;Enderby Basin;Oman ophiolite
AB We analyzed high-quality seismic reflection profiles across the ocean-continent transition in the Enderby Basin between the Kerguelen Plateau and the Antarctic margin. There, we observe numerous high-amplitude dipping reflections in the lower oceanic crust which was accreted at a magmatic spreading center as testified by the almost uniform 6.4-7 km thick crust and its unfaulted, flat top basement. The deep reflections are rooting onto the Moho and are dipping both ridgeward and continentward. They occur in dense networks in mature oceanic crust as well as close to the continentward termination of oceanic crust and in the ocean-continent transition zone. The comparison with field observations in the Oman ophiolite suggests that these lower crustal dipping reflectors could correspond to syn-magmatic faults. In Oman, very high temperature (up to syn-magmatic), high temperature (sub-solidus plastic deformation) and low temperature (brittle) deformation coexist along the same fault over distances of a few hundred meters at Moho level. This very high temperature gradient may be explained by the sudden and intense interaction between crystallizing magmas and hydrothermal fluids induced by the episodic nucleation of faults in a context of continuous magmatic spreading. The igneous layering becomes extremely irregular compared to its monotonous sub-horizontal orientation away from the faults which, together with enhanced hydrothermal alteration restricted to the fault zones, might change the physical properties (velocity, density) and increase the reflectivity of syn-magmatic faults. We further speculate that these processes could explain the brightness of the lower crustal dipping reflectors observed in our seismic reflection data. Both the seismic reflection profiles of the Enderby Basin and the Oman ophiolite show evidence for syn-accretion tectonism at depth together with the systematic rotation of originally horizontal lava flows or originally vertical dikes, pre-dating cessation of magmatic activity. This indicates ubiquitous deformation processes within the axial zone of magmatic spreading centers. 
PY 2021
PD JAN
SO Earth And Planetary Science Letters
SN 0012-821X
PU Elsevier
VL 554
UT 000604582500042
DI 10.1016/j.epsl.2020.116698
ID 88513
ER

EF