GEOLOGICAL INTERPRETATION OF WHOLE-ROCK ISOCHRON DATES FROM HIGH-GRADE GNEISS TERRAINS

被引：21

作者：

MOORBATH, S ^{[1
]}

机构：

[1] OXFORD UNIV,DEPT GEOL & MINERAL,OXFORD,ENGLAND

来源：

NATURE | 1975年 / 255卷 / 5507期

关键词：

D O I：

10.1038/255391a0

中图分类号：

O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];

学科分类号：

07 ; 0710 ; 09 ;

摘要：

引用

页码：391 / 391

页数：1

共 13 条

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[3] GEOCHEMISTRY OF GRANUNITE FACIES ROCKS AND PROBLEMS OF THEIR ORIGIN [J].

HEIER, KS .

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[5]

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[6]

Moorbath, 1975, J GEOL SOC LONDON, V131, P213

[7] EVOLUTION OF PRECAMBRIAN CRUST FROM STRONTIUM ISOTOPIC EVIDENCE [J].

MOORBATH, S .

NATURE, 1975, 254 (5499) :395-398

[8] FURTHER RUBIDIUM-STRONTIUM AGE DETERMINATIONS ON VERY EARLY PRECAMBRIAN ROCKS OF GODTHAAB DISTRICT, WEST GREENLAND [J].

MOORBATH, S ;

GALE, NH ;

PANKHURS.RJ ;

MCGREGOR, VR ;

ONIONS, RK .

NATURE-PHYSICAL SCIENCE, 1972, 240 (100) :78-&

[9] SIGNIFICANCE OF LEAD ISOTOPE STUDIES IN ANCIENT, HIGH-GRADE METAMORPHIC BASEMENT COMPLEXES, AS EXEMPLIFIED BY LEWISIAN ROCKS OF NORTHWEST SCOTLAND [J].

MOORBATH, S ;

WELKE, H ;

GALE, NH .

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[10]

MOORBATH S, EARLY HISTORY EARTH

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