THE ND AND SR ISOTOPIC EVOLUTION OF PROTEROZOIC SEAWATER

被引：54
作者：
DERRY, LA
JACOBSEN, SB
机构：
来源：
GEOPHYSICAL RESEARCH LETTERS | 1988年 / 15卷 / 04期
关键词：
D O I：
10.1029/GL015i004p00397
中图分类号：
P [天文学、地球科学];
学科分类号：
07 ;
摘要：
引用
收藏
页码：397 / 400
页数：4
相关论文
共 22 条
[1]   THE GROWTH OF THE CONTINENT THROUGH GEOLOGICAL TIME STUDIED BY ND ISOTOPE ANALYSIS OF SHALES [J].
ALLEGRE, CJ ;
ROUSSEAU, D .
EARTH AND PLANETARY SCIENCE LETTERS, 1984, 67 (01) :19-34
[2]   EVIDENCE FOR A 150-200-KM THICK ARCHEAN LITHOSPHERE FROM DIAMOND INCLUSION THERMOBAROMETRY [J].
BOYD, FR ;
GURNEY, JJ ;
RICHARDSON, SH .
NATURE, 1985, 315 (6018) :387-389
[3]   VARIATION OF MARINE SR-87-SR-86 RATIO DURING PHANEROZOIC TIME - INTERPRETATION USING A FLUX MODEL [J].
BRASS, GW .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1976, 40 (07) :721-730
[4]  
BURKE WH, 1982, GEOLOGY, V10, P516, DOI 10.1130/0091-7613(1982)10<516:VOSSTP>2.0.CO
[5]  
2
[6]  
FRYER B, 1983, IRON FORMATION FACTS, P345
[7]   THE ND AND SR ISOTOPIC SYSTEMATICS OF RIVER-WATER DISSOLVED MATERIAL - IMPLICATIONS FOR THE SOURCES OF ND AND SR IN SEAWATER [J].
GOLDSTEIN, SJ ;
JACOBSEN, SB .
CHEMICAL GEOLOGY, 1987, 66 (3-4) :245-272
[8]  
Holland H.D., 1984, CHEM EVOLUTION ATMOS
[9]   A ND ISOTOPIC STUDY OF THE HAMERSLEY AND MICHIPICOTEN BANDED IRON FORMATIONS - THE SOURCE OF REE AND FE IN ARCHEAN OCEANS [J].
JACOBSEN, SB ;
PIMENTELKLOSE, MR .
EARTH AND PLANETARY SCIENCE LETTERS, 1988, 87 (1-2) :29-44
[10]  
JACOBSEN SB, 1988, IN PRESS GEOPHYS RES
123