GEOCHRONOLOGICAL SIGNIFICANCE OF DISCORDANT U-PB AGES OF OVAL-SHAPED ZIRCONS FROM A LEWISIAN GNEISS FROM HARRIS, OUTER-HEBRIDES

被引：39

作者：

PIDGEON, RT ^{[1
]}

AFTALION, M ^{[1
]}

机构：

[1] SCOTTISH RES REACTOR CTR,E KILBRIDE,SCOTLAND

来源：

关键词：

D O I：

10.1016/0012-821X(72)90286-5

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：

引用

页码：269 / 274

页数：6

共 18 条

[1] Coward MP., 1969, P GEOL ASS, V80, P387
[2] DEARNLEY R, 1962, Q J GEOL SOC LOND, V118, P143
[3] Dearnley R., 1963, Q J GEOL SOC, V119, P243
[4] Giletti B.J., 1961, Q J GEOL SOC LOND, V117, P233, DOI DOI 10.1144/GSJGS.117.1.0233
[5] Goldich S.S., 1970, GEOL SOC AM BULL, V81, P3671
[6] HOPGOOD AM, 1972, GEOL SOC AM BULL, V83, P107, DOI 10.1130/0016-7606(1972)83[107:AOSSTT]2.0.CO
[7] 2
[8] KOPPEL V, 1971, SCHWEIZ MINER PETROG, V51, P385
[9] LYON TDB, IN PRESS
[10] SIGNIFICANCE OF LEAD ISOTOPE STUDIES IN ANCIENT, HIGH-GRADE METAMORPHIC BASEMENT COMPLEXES, AS EXEMPLIFIED BY LEWISIAN ROCKS OF NORTHWEST SCOTLAND
MOORBATH, S
WELKE, H
GALE, NH
[J]. EARTH AND PLANETARY SCIENCE LETTERS, 1969, 6 (04) : 245 - &