FURTHER EVIDENCE FOR GLACIOGENIC ORIGIN OF LATE PRECAMBRIAN MIXTITES IN ANGOLA

被引：12

作者：

KRONER, A

CORREIA, H

机构：

[1] UNIV CAPE TOWN,PRECAMBRIAN RES UNIT,RONDEBOSCH,SOUTH AFRICA

[2] UNIV LUANDA,DEPT GEOL,CP 815,LUANDA,ANGOLA

来源：

NATURE-PHYSICAL SCIENCE | 1973年 / 246卷 / 155期

关键词：

D O I：

10.1038/physci246115a0

中图分类号：

Q6 [生物物理学];

学科分类号：

071011 ;

摘要：

引用

页码：115 / 117

页数：3

共 50 条

[1] NO EVIDENCE FOR GLACIAL ORIGIN OF LATE PRECAMBRIAN TILLOIDS IN ANGOLA
SCHERMER.LJ
[J]. NATURE, 1974, 252 (5479) : 114 - 115
[2] NO EVIDENCE FOR GLACIAL ORIGIN OF LATE PRECAMBRIAN TILLOIDS IN ANGOLA - REPLY
KRONER, A
[J]. NATURE, 1974, 252 (5479) : 115 - 116
[3] LATE PRECAMBRIAN MIXTITES - GLACIAL AND-OR NONGLACIAL
SCHERMERHORN, LJ
[J]. AMERICAN JOURNAL OF SCIENCE, 1974, 274 (07) : 673 - 824
[4] RECOGNITION OF LATE PRECAMBRIAN GLACIOGENIC SEDIMENTS IN LIBERIA
MAGEE, AW
CULVER, SJ
[J]. GEOLOGY, 1986, 14 (11) : 920 - 922
[5] LATE PRECAMBRIAN MIXTITES - GLACIAL AND/OR NON-GLACIAL - DEALING ESPECIALLY WITH MIXTITES OF WEST-AFRICA
DEYNOUX, M
TROMPETTE, R
[J]. AMERICAN JOURNAL OF SCIENCE, 1976, 276 (10) : 1302 - 1315
[6] LATE PRECAMBRIAN MIXTITES - GLACIAL AND-OR NON-GLACIAL - REPLY
SCHERMERHORN, LJG
[J]. AMERICAN JOURNAL OF SCIENCE, 1976, 276 (03) : 375 - 384
[7] LATE PRECAMBRIAN MIXTITES - GLACIAL AND/OR NON-GLACIAL - DEALING ESPECIALLY WITH MIXTITES OF WEST-AFRICA - REPLY
SCHERMERHORN, LJG
[J]. AMERICAN JOURNAL OF SCIENCE, 1976, 276 (10) : 1315 - 1324
[8] NATURE AND CLASSIFICATION OF WATERLAIN GLACIOGENIC SEDIMENTS, EXEMPLIFIED BY PLEISTOCENE, LATE PALEOZOIC AND LATE PRECAMBRIAN DEPOSITS
GRAVENOR, CP
VONBRUNN, V
DREIMANIS, A
[J]. EARTH-SCIENCE REVIEWS, 1984, 20 (02) : 105 - 166
[9] HEAVY MINERALS AND SEDIMENTOLOGICAL STUDIES ON THE GLACIOGENIC LATE PRECAMBRIAN GASKIERS FORMATION OF NEWFOUNDLAND
GRAVENOR, CP
[J]. CANADIAN JOURNAL OF EARTH SCIENCES, 1980, 17 (10) : 1331 - 1341
[10] PALEOMAGNETIC RESULTS FROM THE LATE PRECAMBRIAN CHELA GROUP OF SOUTHWEST ANGOLA
JONES, DL
MCFADDEN, PL
KRONER, A
MCWILLIAMS, MO
[J]. PRECAMBRIAN RESEARCH, 1992, 59 (1-2) : 1 - 13

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