ISOTOPIC COMPOSITION OF LEAD FROM PINE POINT DEPOSIT

被引:16
作者
CUMMING, GL
ROBERTSO.DK
机构
[1] Department of Geology, University of Alberta, Edmonton, AB
关键词
D O I
10.2113/gsecongeo.64.7.731
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
Preliminary lead isotope ratios on nine samples from the Pine Point area are reported. The ratios are consistent within the experimental errors of about 0.25% and fall on the mantle growth curve. They indicate that the lead came from a homogeneous source with a model age of about 250-275 million years, appreciably younger than the Devonian host rocks. © 1969 Society of Economic Geologists, Inc.
引用
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页码:731 / &
相关论文
共 4 条
[1]  
FARQUHAR RM, 1954, T ROY SOC CAN 3, V48, P9
[2]  
Kanasewich E.R, 1968, RADIOMETRIC DATING G, P147
[3]  
OSTIC RG, 1967, CAN J EARTH SCI, V4, P245
[4]   SULFUR ISOTOPES AND PINE POINT LEAD-ZINC MINERALIZATION [J].
SASAKI, A ;
KROUSE, HR .
ECONOMIC GEOLOGY, 1969, 64 (07) :718-&