Evaluating reference materials and common-Pb corrections for high-resolution apatite U-Pb geochronology

被引:0
|
作者
Apen, Francisco E. [1 ]
Gaynor, Sean P. [1 ]
Schoene, Blair [1 ]
Cottle, John M. [2 ]
机构
[1] Princeton Univ, Dept Geosci, Princeton, NJ 08544 USA
[2] Univ Calif Santa Barbara, Dept Earth Sci, Santa Barbara, CA 93106 USA
关键词
Apatite; U-Pb; Geochronology; Thermochronology; ID-TIMS; LA-ICP-MS; JUAN VOLCANIC FIELD; FISH CANYON TUFF; PLASMA-MASS SPECTROMETRY; K-40 DECAY CONSTANTS; TRACE-ELEMENT; ID-TIMS; THERMAL EVOLUTION; DULUTH COMPLEX; ICP-MS; METASOMATIC PROCESSES;
D O I
10.1016/j.chemgeo.2024.122191
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We report isotope dilution thermal ionization mass spectrometry (ID-TIMS) and laser ablation split stream inductively coupled plasma mass spectrometry (LASS) U - Pb data for a suite of widely available reference apatites: Fish Canyon Tuff, Mount Dromedary, TEMORA 2, and Duluth Complex anorthosite. We apply different common-Pb correction strategies to the U - Pb data sets: (1) anchoring to a Stacey and Kramers (1975) model Pb composition; (2) unanchored 2-D 238 U/ 206 Pb- 207 Pb/ 206 Pb isochron regressions; and (3) unanchored 3-D 238 U/ 206 Pb- 207 Pb/ 206 Pb- 204 Pb/ 206 Pb isochron regressions. The different common-Pb corrections yield consistent dates within each ID-TIMS and LASS data set, with 3-D regression method producing the highest precision isochrons. FCT apatite produces an ID-TIMS 3-D isochron age of 28.8 +/- 3.7 Ma with ( 207 Pb/ 206 Pb) i = 0.851 +/- 0.021. Mount Dromedary apatite yields an ID-TIMS 3-D isochron age of 98.4 +/- 0.5 Ma with ( 207 Pb/ 206 Pb) i = 0.839 +/- 0.003. TEMORA 2 apatite has an ID-TIMS 3-D isochron age of 402 +/- 7 Ma and ( 207 Pb/ 206 Pb) i = 0.839 +/- 0.008. Duluth Complex anorthosite apatite yields an ID-TIMS 3-D isochron age of 1077 +/- 9 Ma with ( 207 Pb/ 206 Pb) i = 0.849 +/- 0.046. The MSWDs associated with isochrons calculated from both the ID-TIMS and LASS data sets are larger than expected for a single age population, revealing complexities that are otherwise not captured by 2-D isochron methods. In the case of FCT apatite, the ID-TIMS data indicate significant heterogeneity in the initial Pb ratio (( 207 Pb/ 206 Pb) i = 0.845-0.856), invalidating this sample as a viable reference apatite for high -precision geochronology. Additionally, the common-Pb compositions of TEMORA 2 and Duluth Complex anorthosite apatites calculated using the ID-TIMS data deviate from bulk Earth Pb evolution models beyond 2 sigma uncertainty. The data emphasize the utility of unanchored age regressions in generating the highest fidelity apatite U - Pb dates. Further, TEMORA 2 and Duluth Complex apatite ages are both younger than their corresponding zircon U - Pb ages, highlighting the need to independently verify the ages of prospective reference apatites.
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页数:13
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