THE SCOURIE DYKE SUITE - PETROGENESIS AND GEOCHEMICAL NATURE OF THE PROTEROZOIC SUB-CONTINENTAL MANTLE

被引：131

作者：

WEAVER, BL

TARNEY, J

机构：

来源：

CONTRIBUTIONS TO MINERALOGY AND PETROLOGY | 1981年 / 78卷 / 02期

关键词：

D O I：

10.1007/BF00373779

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：175 / 188

页数：14

共 68 条

[1] ISOTOPIC AND CHEMICAL EFFECTS PRODUCED IN A CONTINUOUSLY DIFFERENTIATING CONVECTING EARTH MANTLE [J].

ALLEGRE, CJ ;

BREVART, O ;

DUPRE, B ;

MINSTER, JF .

PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES, 1980, 297 (1431) :447-477

[2] ORIGIN OF PHLOGOPITE AND POTASSIC RICHTERITE BEARING PERIDOTITE XENOLITHS FROM SOUTH-AFRICA [J].

AOKI, K .

CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 1975, 53 (03) :145-156

[3]

ARTH JG, 1976, J RES US GEOL SURV, V4, P41

[4] MAJOR AND TRACE-ELEMENT PATTERNS ESTABLISHED DURING RETROGRESSIVE METAMORPHISM OF GRANULITE-FACIES GNEISSES, NW SCOTLAND [J].

BEACH, A ;

TARNEY, J .

PRECAMBRIAN RESEARCH, 1978, 7 (04) :325-348

[5] CONTRASTING TYPES OF CHROMIUM-SPINEL PERIDOTITE XENOLITHS IN BASANITIC LAVAS, WESTERN GRAND-CANYON, ARIZONA [J].

BEST, MG .

EARTH AND PLANETARY SCIENCE LETTERS, 1974, 23 (02) :229-237

[6] EVIDENCE FOR VARIABILITY OF MAGMATIC PROCESSES AND UPPER MANTLE HETEROGENEITY IN THE AXIAL REGION OF THE MID-ATLANTIC RIDGE NEAR 22-DEGREES AND 36-DEGREES-N [J].

BOUGAULT, H ;

CAMBON, P ;

CORRE, O ;

JORON, JL ;

TREUIL, M .

TECTONOPHYSICS, 1979, 55 (1-2) :11-34

[7] 2,390 MYR RB-SR WHOLE-ROCK FOR THE SCOURIE DYKES OF NORTHWEST SCOTLAND [J].

CHAPMAN, HJ .

NATURE, 1979, 277 (5698) :642-643

[8] INFERENCES ABOUT MAGMA SOURCES AND MANTLE STRUCTURE FROM VARIATIONS OF ND-143-ND-144 [J].

DEPAOLO, DJ ;

WASSERBURG, GJ .

GEOPHYSICAL RESEARCH LETTERS, 1976, 3 (12) :743-746

[9]

DUNCAN RA, 1980, GEOLOGY, V8, P22, DOI 10.1130/0091-7613(1980)8<22:ROMMIT>2.0.CO

[10]

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