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

被引:3
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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共 107 条
[1]   Apatites for destruction: Reference apatites from Morocco and Brazil for U-Pb petrochronology and Nd and Sr isotope geochemistry [J].
Apen, Francisco E. ;
Wall, Corey J. ;
Cottle, John M. ;
Schmitz, Mark D. ;
Kylander-Clark, Andrew R. C. ;
Seward, Gareth G. E. .
CHEMICAL GEOLOGY, 2022, 590
[2]   Four-dimensional thermal evolution of the East African Orogen: accessory phase petrochronology of crustal profiles through the Tanzanian Craton and Mozambique Belt, northeastern Tanzania [J].
Apen, Francisco E. ;
Rudnick, Roberta L. ;
Cottle, John M. ;
Kylander-Clark, Andrew R. C. ;
Blondes, Madalyn S. ;
Piccoli, Philip M. ;
Seward, Gareth .
CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 2020, 175 (11)
[3]   40Ar/39Ar and U-Pb dating of the Fish Canyon magmatic system, San Juan Volcanic field, Colorado: Evidence for an extended crystallization history [J].
Bachmann, O. ;
Oberli, F. ;
Dungan, M. A. ;
Meier, M. ;
Mundil, R. ;
Fischer, H. .
CHEMICAL GEOLOGY, 2007, 236 (1-2) :134-166
[4]   Rejuvenation of the Fish Canyon magma body: A window into the evolution of large-volume silicic magma systems [J].
Bachmann, O ;
Bergantz, GW .
GEOLOGY, 2003, 31 (09) :789-792
[5]   Warm storage for arc magmas [J].
Barboni, Melanie ;
Boehnke, Patrick ;
Schmitt, Axel K. ;
Harrison, T. Mark ;
Shane, Phil ;
Bouvier, Anne-Sophie ;
Baumgartner, Lukas .
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 2016, 113 (49) :13959-13964
[6]   Behavior of accessory phases and redistribution of Zr, REE, Y, Th, and U during metamorphism and partial melting of metapelites in the lower crust: An example from the Kinzigite Formation of Ivrea-Verbano, NW Italy [J].
Bea, F ;
Montero, P .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1999, 63 (7-8) :1133-1153
[7]   Thermal history and origin of the Tanzanian Craton from Pb isotope thermochronology of feldspars from lower crustal xenoliths [J].
Bellucci, Jeremy J. ;
McDonough, William F. ;
Rudnick, Roberta L. .
EARTH AND PLANETARY SCIENCE LETTERS, 2011, 301 (3-4) :493-501
[8]   Apatite as an indicator mineral for mineral exploration: trace-element compositions and their relationship to host rock type [J].
Belousova, EA ;
Griffin, WL ;
O'Reilly, SY ;
Fisher, NI .
JOURNAL OF GEOCHEMICAL EXPLORATION, 2002, 76 (01) :45-69
[9]   Improved 206Pb/238U microprobe geochronology by the monitoring of a trace-element-related matrix effect; SHRIMP, ID-TIMS, ELA-ICP-MS and oxygen isotope documentation for a series of zircon standards [J].
Black, LP ;
Kamo, SL ;
Allen, CM ;
Davis, DW ;
Aleinikoff, JN ;
Valley, JW ;
Mundil, R ;
Campbell, IH ;
Korsch, RJ ;
Williams, IS ;
Foudoulis, C .
CHEMICAL GEOLOGY, 2004, 205 (1-2) :115-140
[10]  
Boesen R.S., 1972, J. Geol. Soc. Aust., V19, P345, DOI [10.1080/00167617208728802, DOI 10.1080/00167617208728802]