2006 Philadelphia Annual Meeting (22–25 October 2006)

Paper No. 1
Presentation Time: 1:45 PM

DETRITAL ZIRCON U-TH-PB GEOCHRONOLOGY BY LA-MC-ICPMS AT THE ARIZONA LASERCHRON CENTER


GEHRELS, George E.1, RUIZ, Joaquin1, VALENCIA, Victor A.2, PULLEN, Alexander3 and BAKER, Mark1, (1)Department of Geosciences, University of Arizona, Tucson, AZ 85721, (2)Geosciences, Univ of Arizona, 1040 E Fourth Street, Tucson, AZ 85721-0077, (3)Geosciences, Univ of Arizona, Tucson, AZ 85721, ggehrels@geo.arizona.edu

The Arizona LaserChron Center (www.geo.arizona.edu/alc) utilizes a 193 nm excimer laser system (from Lambda Physik and New Wave Research) and a multicollector ICPMS (from GV Instruments) to conduct U-Th-Pb geochronologic analyses. This instrument is ideally suited for detrital zircon analyses because it has a rapid throughput (40 unknowns per hour), yields ages with a precision of 1-2% (2-sigma) for a single analysis and an accuracy of 1% for a set of 10 or more analyses, can measure 204 accurately, yields robust U/Th petrogenetic information, and has a spatial resolution down to 15 by 10 microns (pit width by depth). Our typical strategy for detrital samples is to analyze 100 zircon grains (selected at random) using a beam size appropriate for analysis of the smallest grains in the sample. Ages are calibrated relative to fragments of a Sri Lanka zircon grain that is calibrated by ID-TIMS and is cross-calibrated relative to R33, Temora, 91500, and FC-1. Standards are analyzed once every five unknowns, and each unknown is calibrated relative to 206/238, 208/232, and 206/207 of the closest six standard analyses. The resulting ages are plotted on relative age probability plots according to 206/238 ages (for <1.0 Ga grains) or 206/207 ages (for >1.0 Ga grains), and significance is attached only to age peaks that comprise three or more analyses. This is because clustering of ages is a more robust indicator of reliability than concordance or precision, but this strategy precludes attributing significance to an individual analysis and especially to the youngest grain in a sample.

The Arizona LaserChron Center is funded by the NSF/EAR Instrumentation and Facilities Program to operate as a multi-user facility, with ~50% subsidy of analytical costs for NSF-supported research. This yields a user cost of $400 for analysis of 100 unknowns. Additional support for student use is also provided by NSF. This style of operation is having a significant impact on provenance studies given that we currently generate ~40,000 detrital zircon ages for ~50 projects per year.