3D development of detachment faulting during continental breakup

被引:45
作者
Lymer, Gael [1 ]
Cresswell, Derren J. F. [1 ]
Reston, Tim J. [1 ]
Bull, Jonathan M. [2 ]
Sawyer, Dale S. [3 ]
Morgan, Julia K. [3 ]
Stevenson, Carl [1 ]
Causer, Annabel [1 ]
Minshull, Tim A. [2 ]
Shillington, Donna J. [4 ]
机构
[1] Univ Birmingham, Sch Geog Earth & Environm Sci, Birmingham, W Midlands, England
[2] Univ Southampton, Sch Ocean & Earth Sci, Southampton, Hants, England
[3] Rice Univ, Dept Earth Sci, Houston, TX USA
[4] Lamont Doherty Earth Observ, Palisades, NY USA
基金
英国自然环境研究理事会; 美国国家科学基金会;
关键词
rifting processes; Galicia margin; North Atlantic Ocean; detachment fault; asymmetry; 3D seismic reflection; FLEMISH CAP; LITHOSPHERIC EXTENSION; CONJUGATE MARGINS; EVOLUTION; MANTLE; SEA; SERPENTINIZATION; SERPENTINISATION; STRENGTH; ROTATION;
D O I
10.1016/j.epsl.2019.03.018
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The developing asymmetry of rifting and continental breakup to form rifted margins has been much debated, as has the formation, mechanics and role of extensional detachments. Bespoke 3D seismic reflection data across the Galicia margin, west of Spain, image in unprecedented detail an asymmetric detachment (the S reflector). Mapping S in 3D reveals its surface is corrugated, proving that the overlying crustal blocks slipped on S surface during the rifting. Crucially, the 3D data show that the corrugations on S perfectly match the corrugations observed on the present-day block-bounding faults, demonstrating that S is a composite surface, comprising the juxtaposed rotated roots of block-bounding faults as in a rolling hinge system with each new fault propagation moving rifting oceanward; changes in the orientation of the corrugations record the same oceanward migration. However, in contrast to previous rolling hinge models, the slip of the crustal blocks on S occurred at angles as low as 20, requiring that S was unusually weak, consistent with the hydration of the underlying mantle by seawater ingress following the embrittlement of the entire crust. As the crust only becomes entirely brittle once thinned to 10 km, the asymmetric S detachment and the hyper-extension of the continental crust only developed late in the rifting process, which is consistent with the observed development of asymmetry between conjugate magma poor margin pairs. The 3D volume allows analysis of the heaves and along strike architecture of the normal faults, whose planes laterally die or spatially link together, implying overlaps in faults activity during hyper-extension. Our results thus reveal for the first time the 3D mechanics and timing of detachment faulting growth, the relationship between the detachment and the network of block-bounding faults above it and the key processes controlling the asymmetrical development of conjugate rifted margins. (C) 2019 Elsevier B.V. All rights reserved.
引用
收藏
页码:90 / 99
页数:10
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