Inherited Crustal Features and Southern Alaska Tectonic History Constrained by Sp Receiver Functions
Ruppert, Natalia A; Jadamec, Margarete A; Freymueller, Jeffrey T
(Ed.)
Southern Alaska is a collage of accreted terranes. The deformation history of accreted terranes and the geometric history of their bounding faults reflect both inherited features and associated convergent margin events. We employ S-to-P receiver functions on multiple dense (<20km spacing) arrays of broadband seismometers across southern Alaska to investigate signals of dynamic tectonic activity. An inboard-dipping (∼15∘) boundary is imaged aligning with the trace of the Border Ranges Fault, which is interpreted as an unrotated inboard-dipping paleo-subduction (Mesozoic) interface. This observation, along with previous seismic imaging of the Border Ranges Fault and the next outboard terrane-bounding fault, the Contact Fault, buttresses a known history of convergent tectonics that varies along the margin. Large (>10 km) crustal thickness offsets imaged across both the Denali Fault system and the Eureka Creek Fault support a Mesozoic-to-Present inboard-dipping (east and northward) subduction polarity in the region. Additionally, our imaging reveals a significant velocity increase with depth at ∼25km beneath the Copper River Basin, which we interpret as the top of a region of active underplating and/or intrusion of basaltic magmatism. This feature may be related to the generation of a newWrangell Volcanic Field volcano, resulting from the underlying tear in the subducting slab.
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