Seafloor overthrusting creates ductilely deformed fault rocks in marine sediments at the Hikurangi Margin; implications for fault zone evolution and mechanics at IODP site U1518

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http://abstractsearch.agu.org/meetings/2018/FM/T51I-0301.html
Author(s): Morgan, Julia; Fagereng, Ake; Savage, Heather M.; Wang Maomao; Meneghini, Francesca; Barnes, Philip; Bell, Rebecca E.; Kitajima, Hiroko; Dugan, Brandon; Wallace, Laura M.; Saffer, Demian M.; Pecher, Ingo Andreas; Petronotis, Katerina E.; LeVay, Leah J.
International Ocean Discovery Program (IODP), Expedition 372 Scientists
Author Affiliation(s): Primary:
Rice University, Houston, TX, United States
Other:
University of Cape Town, South Africa
Lamont-Doherty Earth Observatory, United States
Hohai University, China
University of Pisa, Italy
National Institute of Water & Atmospheric Research, New Zealand
Imperial College London, United Kingdom
Texas A & M University, United States
Colorado School of Mines, United States
University of Texas at Austin, United States
Pennsylvania State University, United States
University of Auckland, New Zealand
International Ocean Discovery Program, United States
Volume Title: AGU 2018 fall meeting
Source: American Geophysical Union Fall Meeting, Vol.2018; American Geophysical Union 2018 fall meeting, Washington, DC, Dec. 10-14, 2018. Publisher: American Geophysical Union, Washington, DC, United States
Note: In English
Summary: IODP Site U1518, drilled during Exp 372 and 375, penetrated a major thrust fault rising from a megathrust that experiences slow slip along the Hikurangi margin. This thrust fault has hosted >4 km of displacement. Although intersected at only ∼0 mbsf within moderate porosity clay-rich sediments, the fault zone exhibits intense tectonic ductile deformation with characteristics of crustal shear zones, including (1) finely banded mudstones, contorted into decimeter-scale folds; (2) elongate mudstone clasts with grain tail complexes; (3) stacked and truncated silt beds in distorted mudstones; and (4) soft sediment injections. Locally, these ductile features are overprinted by brittle structures, including normal faults, fracture arrays, and breccias. The wall rocks also exhibit ductile deformation, including shear banding, asymmetric clasts, and injection features. The hanging wall exhibits a brittle overprint, with small-offset normal faults and locally pervasive filled fractures, increasing in intensity toward to the fault. Brittle deformation is less common and more localized in the footwall. Intense tectonically-derived ductile deformation has not been reported in previously drilled accretionary faults, but can be readily explained by the kinematics of this thrust fault. The large offset along this fault requires that the hanging wall overthrusted the seafloor. Thus, at Site U1518 a hanging wall ramp was superimposed upon a footwall flat trapping high porosity, undeformed, and previously unburied sediments beneath the fault zone. The porous sediments underwent ductile shearing during hanging wall emplacement, and fluidized under low effective stresses, injecting into more cohesive wall rocks. Fault kinematics also explain the asymmetry in deformation: hanging wall strata underwent folding and brittle deformation as they moved through kink folds above the fault bend. In contrast, footwall strata retained their planar orientations and experienced primarily ductile compaction. Over time, pore fluids were expelled and sediments consolidated under the hanging wall load, causing progressive strengthening of the fault zone. The kinematic and mechanical evolution of this frontal thrust has implications for fault zone processes today in response to slow slip along the megathrust fault.
Year of Publication: 2018
Research Program: IODP Integrated Ocean Drilling Program
IODP2 International Ocean Discovery Program
Key Words: 16 Structural Geology; Deformation; Ductility; Expedition 372; Expedition 375; Fault zones; Faults; Hikurangi Margin; IODP Site U1518; International Ocean Discovery Program; Ocean floors; Overthrust faults; Pacific Ocean; South Pacific; Southwest Pacific; Tectonics; West Pacific
Coordinates: S385133 S385133 E1785346 E1785346
Record ID: 2019050432
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