Thermal events documented in Hadean zircons by ion microprobe depth profiles

被引:56
作者
Trail, Dustin
Mojzsis, Stephen J.
Harrison, T. Mark
机构
[1] Univ Colorado, Dept Geol Sci, Boulder, CO 80309 USA
[2] Univ Colorado, Ctr Astrobiol, Boulder, CO 80309 USA
[3] Australian Natl Univ, Res Sch Earth Sci, Canberra, ACT 0200, Australia
[4] Univ Calif Los Angeles, Dept Earth & Space Sci, Los Angeles, CA 90095 USA
[5] Univ Calif Los Angeles, Inst Geophys & Planetary Phys, Los Angeles, CA 90095 USA
基金
美国国家科学基金会; 美国国家航空航天局; 澳大利亚研究理事会;
关键词
D O I
10.1016/j.gca.2007.06.003
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 the first U-Th-Pb ion microprobe depth profiles of four Hadean zircons from the Jack Hills and Mount Narryer supracrustal belts of the Narryer Gneiss Complex (NGC), Western Australia. This ultra-bigh spatial resolution technique probes the age and origin of sub-micron features in individual crystals that can record episodes of zircon growth. Near-surface grain dates of 2700 Ma or older are coincident with post-depositional growth/modification. Some ages may coincide with documented pre-deposition metamorphic events for the NGC and igneous emplacement at ca. 3700 Ma. Separate events that do not correlate in time with known geologic episodes prior to the preserved rock record are also present on pre-4000 Ma zircons. We find evidence for a similar to 3.9 Ga event, which is coterminous within age uncertainty with one or several large basin-forming impacts (e.g. Nectaris) on the Moon attributed to the late heavy bombardment of the inner solar system. (c) 2007 Elsevier Ltd. All rights reserved.
引用
收藏
页码:4044 / 4065
页数:22
相关论文
共 101 条
[1]   Nature of the Earth's earliest crust from hafnium isotopes in single detrital zircons [J].
Amelin, Y ;
Lee, DC ;
Halliday, AN ;
Pidgeon, RT .
NATURE, 1999, 399 (6733) :252-255
[2]   Sm-Nd systematics of zircon [J].
Amelin, Y .
CHEMICAL GEOLOGY, 2004, 211 (3-4) :375-387
[3]   Geochronology of the Jack hills detrital zircons by precise U-Pb isotope dilution analysis of crystal fragments [J].
Amelin, YV .
CHEMICAL GEOLOGY, 1998, 146 (1-2) :25-38
[4]   Extraterrestrial iridium, sediment accumulation and the habitability of the early Earth's surface [J].
Anbar, AD ;
Zahnle, KJ ;
Arnold, GL ;
Mojzsis, SJ .
JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS, 2001, 106 (E2) :3219-3236
[5]  
[Anonymous], ACCRETION EXTRATERRE
[6]   RADIOGENIC ISOTOPES - THE CASE FOR CRUSTAL RECYCLING ON A NEAR-STEADY-STATE NO-CONTINENTAL-GROWTH EARTH [J].
ARMSTRONG, RL .
PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES, 1981, 301 (1461) :443-472
[7]   THE PERSISTENT MYTH OF CRUSTAL GROWTH [J].
ARMSTRONG, RL .
AUSTRALIAN JOURNAL OF EARTH SCIENCES, 1991, 38 (05) :613-630
[8]   A 4-Gyr shock age for a Martian meteorite and implications for the cratering history of Mars [J].
Ash, RD ;
Knott, SF ;
Turner, G .
NATURE, 1996, 380 (6569) :57-59
[9]   Slow cooling of deep crustal granulites and Pb-loss in zircon [J].
Ashwal, LD ;
Tucker, RD ;
Zinner, EK .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1999, 63 (18) :2839-2851
[10]   THE ORIGIN OF THE MOON AND THE SINGLE-IMPACT HYPOTHESIS .1. [J].
BENZ, W ;
SLATTERY, WL ;
CAMERON, AGW .
ICARUS, 1986, 66 (03) :515-535