Auxiliary Material Submission for Paper 2009tc002541

Intermediate to felsic middle crust in the accreted Talkeetna arc, the Alaska Peninsula, 
and Kodiak Island, south central Alaska: 
An analogue for low-velocity middle crust in modern arcs

Matthew Rioux
Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of 
Technology, Cambridge, Massachusetts, USA

James Mattinson and Bradley Hacker
Department of Earth Science, University of California, Santa Barbara, California, USA


Peter Kelemen
Lamont Doherty Earth Observatory, Columbia University, Palisades, New York, USA

Jurek Blusztajn and Karen Hanghoj
Department of Geology and Geophysics, Woods Hole Oceanographic Institute, Woods 
Hole, Massachusetts, USA

George Gehrels
Department of Geosciences, University of Arizona, Tucson, Arizona, USA

Rioux, M., J. Mattinson, B. Hacker, P. Kelemen, J. Blusztajn, K. Hanghoj, and 
G. Gehrels (2010), Intermediate to felsic middle crust in the accreted Talkeetna 
arc, the Alaska Peninsula, and Kodiak Island, south central Alaska: An analogue 
for low-velocity middle crust in modern arcs, Tectonics, 29, TC3001, 
doi:10.1029/2009TC002541.

Introduction

Auxiliary materials for this article include multi-grain chemical abrasion TIMS U-Pb 
zircon data collected at the University of California, Santa Barbara (Data Set S1; 
2009tc002541-ds01.txt), LA-ICP-MS U-Pb zircon data collected at the University of 
Arizona (Data Set S2; 2009tc002541-ds02.txt), and a table of modal mineralogies used in the 
calculation of sample seismic velocities (Table S1; 2009tc002541-ds03.txt), and a list of 
references cited in the auxiliary tables. The auxiliary data sets and table are tab delimited 
text files created in Microsoft Excel.

1. 2009tc002541-ds01.txt, 2009tc002541-ds01.xls Data Set S1. Multi-grain chemical abrasion-TIMS U-Pb zircon data 

2. 2009tc002541-ds02.txt, 2009tc002541-ds02.xls Data Set S2. Laser ablation-ICP-MS U-Pb zircon data 

3. 2009tc002541-ts01.txt, 2009tc002541-ts01.xls Table S1. Modal mineralogies used to calculate seismic velocities 


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