U-Pb zircon ages from the southwestern Karoo Basin, South Africa-Implications for the Permian-Triassic boundary

被引:87
作者
Fildani, Andrea [1 ]
Weislogel, Amy [2 ]
Drinkwater, Nicholas J. [3 ]
McHargue, Tim [1 ]
Tankard, Anthony
Wooden, Joe [4 ]
Hodgson, David [5 ]
Flint, Stephen [5 ]
机构
[1] Chevron Energy Technol Co, San Ramon, CA 94583 USA
[2] Univ Alabama, Dept Geol Sci, Tuscaloosa, AL 35487 USA
[3] Chevron So African Business Unit, Houston, TX 77002 USA
[4] Stanford Univ, Stanford US Geol Survey Microanal Ctr, Stanford, CA 94305 USA
[5] Univ Liverpool, Dept Earth & Ocean Sci, STRAT Grp, Liverpool L69 3GP, Merseyside, England
关键词
EVENT BED; EVOLUTION; GEOCHRONOLOGY; TANQUA; EXTINCTION; SYSTEMS;
D O I
10.1130/G25685A.1
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
U-Pb ages determined using sensitive high-resolution ion microprobe-reverse geometry on 205 single-grain zircons from 16 ash beds within submarine fan deposits of the Ecca Group provide the first evidence of a marine Permian-Triassic (P-T) boundary in the Karoo Basin of South Africa. These U-Pb ages provide an objective basis for correlating the deep-marine sediments of the southwest Karoo Basin with fluvial-deltaic deposits in the central and eastern parts of the basin where the P-T boundary is recorded in a diverse macrofauna. Furthermore, these new zircon ages and their correlation imply asymmetric subsidence and variable sedimentation rates across the basin.
引用
收藏
页码:719 / 722
页数:4
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