AMS radiocarbon dating of lacustrine sediment from an impact crater in northeastern China

被引：5

作者：

Liu, K. X. ^{[1
,2
]}

Chen, M. ^{[4
]}

Ding, X. F. ^{[1
,2
]}

Fu, D. P. ^{[1
,2
]}

Ding, P. ^{[3
]}

Shen, C. D. ^{[3
]}

Xiao, W. S. ^{[4
]}

机构：

[1] Peking Univ, State Key Lab Nucl Phys & Technol, Beijing 100871, Peoples R China

[2] Peking Univ, Inst Heavy Ion Phys, Sch Phys, Beijing 100871, Peoples R China

[3] Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou 510640, Guangdong, Peoples R China

[4] Chinese Acad Sci, Guangzhou Inst Geochem, Key Lab Mineral & Metallogeny, Guangzhou 510640, Guangdong, Peoples R China

来源：

NUCLEAR INSTRUMENTS & METHODS IN PHYSICS RESEARCH SECTION B-BEAM INTERACTIONS WITH MATERIALS AND ATOMS | 2013年 / 294卷

关键词：

Impact crater; AMS; Radiocarbon; Lacustrine sediment; METEORITE CRATERS; XIUYAN CRATER; AGE; ESTONIA;

D O I：

10.1016/j.nimb.2012.08.043

中图分类号：

TH7 [仪器、仪表];

学科分类号：

0804 ; 080401 ; 081102 ;

摘要：

In order to investigate the origin and age of a bowl-shaped crater with 1.8 km diameter in northeastern China, a core drilling about 110 m in total was carried out in 2009 at the center of the crater. A 106-m-thick unit of lacustrine sediment is revealed under a surface layer of about 1 m of yellow soil. The impact origin has been confirmed based on geological analysis. In this paper, we report the AMS C-14 dating results of lacustrine sediment. The data suggest that the meteorite impact in Xiuyan happened more than 50,000 years ago and a two-section linear relationship of C-14 ages with the depth shows a stable sediment environment through the two time stages. (C) 2012 Elsevier B.V. All rights reserved.

引用

页码：593 / 596

页数：4

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