The age of Wolfe Creek meteorite crater (Kandimalal), Western Australia

被引:6
|
作者
Barrows, Timothy T. [1 ,2 ]
Magee, John [3 ]
Miller, Gifford [4 ,5 ]
Fifield, L. Keith [6 ]
机构
[1] Univ Wollongong, Sch Earth & Environm Sci, Wollongong, NSW 2522, Australia
[2] Univ Portsmouth, Dept Geog, Portsmouth PO1 2UP, Hants, England
[3] Australian Natl Univ, Res Sch Earth Sci, Canberra, ACT 0200, Australia
[4] Univ Colorado, INSTAAR, Boulder, CO 80309 USA
[5] Univ Colorado, Dept Geol Sci, Boulder, CO 80309 USA
[6] Australian Natl Univ, Res Sch Phys & Engn, Dept Nucl Phys, Canberra, ACT 2601, Australia
基金
澳大利亚研究理事会;
关键词
IMPACT CRATERS; EXPOSURE AGES; BE-10; HISTORY; RATES; LUMINESCENCE; ARIZONA;
D O I
10.1111/maps.13378
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
Wolfe Creek crater lies in northwestern Australia at the edge of the Great Sandy Desert. Together with Meteor Crater, it is one of the two largest craters on Earth from which meteorite fragments have been recovered. The age of the impact is poorly constrained and unpublished data places the event at about 300,000 years ago. In comparison, Meteor Crater is well constrained by exposure dating. In this paper, we present new ages for Wolfe Creek Crater from exposure dating using the cosmogenic nuclides Be-10 and Al-26, together with optically stimulated luminescence ages (OSL) on sand from a site created by the impact. We also present a new topographic survey of the crater using photogrammetry. The exposure ages range from similar to 86 to 128 ka. The OSL ages indicate that the age of the impact is most likely to be similar to 120 ka with a maximum age of 137 ka. Considering the geomorphic setting, the most likely age of the crater is 120 +/- 9 ka. Last, we review the age of Meteor Crater in Arizona. Changes in production rates and scaling factors since the original dating work revise the impact age to 61.1 +/- 4.8 ka, or similar to 20% older than previously reported.
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页码:2686 / 2697
页数:12
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