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Large-scale pseudotachylytes and fluidized cataclasites from an ancient subduction thrust fault

¹ Earth Science Department, University of California–Santa Cruz, 1156 High Street, Santa Cruz, California 95064, USA
² Dipartimento di Scienze della Terra, Università di Pisa, via S. Maria, 53, 56126 Pisa, Italy
³ Department of Geosciences, Pennsylvania State University, 320 Deike Building, University Park, Pennsylvania 16802, USA

In the Kodiak accretionary complex, Kodiak Island, Alaska, pseudotachylyte occurs in black, locally vitreous ultrafine-grained fault rock. Microscopic observations show that the pseudotachylytes are composed of glass, with vesicles, amygdules, microlites, and flow structures, indicating a frictional melt. The pseudotachylyte is gradational to cataclasite and shows outcrop-scale injection and ductile deformation structures. The cataclasite was ductily mobile (i.e., fluidized) simultaneous with the formation and emplacement of pseudotachylyte melt. The pseudotachylytic rocks postdate the stratal disruption fabric of associated shear-zone mélanges and show similar direction of thrust transport, and have undergone limited subsequent deformation. We interpret the stratal disruption as resulting from underthrusting of the subducting plate and pseudotachylyte development as the final activity of this thrust surface. The gradational contacts between pseudotachylyte and cataclasite demonstrate that the cataclasite also formed as a seismic product and may represent paleoseismic rupture zones, possibly of very great earthquakes, with or without accompanying pseudotachylytes. The pseudotachylytes are voluminous, and many are spatially disconnected from generation surfaces. This style is distinct from pseudotachylytes described in other environments, and this may explain the rarity of documented examples of subduction-thrust pseudotachylyte.

Key Words: pseudotachylyte • Kodiak accretionary complex • subduction thrust • paleoseismicity • fluidized gouge • cataclasite

This article has been cited by other articles:

				G. B. Piccardo, G. Ranalli, and L. Guarnieri Seismogenic Shear Zones in the Lithospheric Mantle: Ultramafic Pseudotachylytes in the Lanzo Peridotite (Western Alps, NW Italy) J. Petrology, November 6, 2009; (2009) egp067v1. [Abstract] [Full Text] [PDF]