Limitation on the mass exchange between the upper and lower mantle: the evolving convection regime of the Earth

被引:69
作者
Allegre, CJ
机构
关键词
mass exchange; two-layer mantle;
D O I
10.1016/S0012-821X(97)00072-1
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
It is increasingly accepted, through the use of geochemical arguments, that the Earth's mantle has a two-layer structure, comprising an upper and lower mantle. Estimates of the exchange of matter and energy between these two layers are, thus, central to understanding the dynamics of the Earth. Geochemical mass balance permits us to estimate the average flux of exchange between the lower and upper mantle. This estimate can be made using two different classes of chemical tracers: the Lit isotopic systems and the rare gas isotopic system. The absolute values and comparison between these tracers argues for: 1. a limited exchange rate between the lower and upper mantle, the average rate over 4.5 x 10(9) yr being less than 10% of the present-day subduction rate, S; 2. from comparison of these values with the seismic evidence of slab penetration, two-layer convection having operated for most of the Earth's history, but whole mantle convection having started less than 1 billion years ago. We are presently in a transitional stage between these two modes of operation. (C) 1997 Elsevier Science B.V.
引用
收藏
页码:1 / 6
页数:6
相关论文
共 44 条
[1]   CHEMICAL-STRUCTURE AND EVOLUTION OF THE MANTLE AND CONTINENTS DETERMINED BY INVERSION OF ND AND SR ISOTOPIC DATA .2. NUMERICAL EXPERIMENTS AND DISCUSSION [J].
ALLEGRE, CJ ;
HART, SR ;
MINSTER, JF .
EARTH AND PLANETARY SCIENCE LETTERS, 1983, 66 (1-3) :191-213
[2]   The Argon constraints on mantle structure. [J].
Allegre, CJ ;
Hofmann, A ;
ONions, K .
GEOPHYSICAL RESEARCH LETTERS, 1996, 23 (24) :3555-3557
[3]   IMPLICATIONS OF A 2-COMPONENT MARBLE-CAKE MANTLE [J].
ALLEGRE, CJ ;
TURCOTTE, DL .
NATURE, 1986, 323 (6084) :123-127
[4]   CHEMICAL-STRUCTURE AND HISTORY OF THE EARTH - EVIDENCE FROM GLOBAL NON-LINEAR INVERSION OF ISOTOPIC DATA IN A 3-BOX MODEL [J].
ALLEGRE, CJ ;
LEWIN, E .
EARTH AND PLANETARY SCIENCE LETTERS, 1989, 96 (1-2) :61-88
[5]  
ALLEGRE CJ, THEORETICAL METHOD 1, V66
[6]   PHASE-TRANSITION CLAPEYRON SLOPES AND TRANSITION ZONE SEISMIC DISCONTINUITY TOPOGRAPHY [J].
BINA, CR ;
HELFFRICH, G .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 1994, 99 (B8) :15853-15860
[7]  
BOEHLER R, 1992, HIGH PRESSURE RES AP, P55
[8]   LAYERED CONVECTION INDUCED BY PHASE-TRANSITIONS [J].
CHRISTENSEN, UR ;
YUEN, DA .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1985, 90 (NB12) :291-300
[9]   EXCESS HE-3 IN DEEP-WATER ON EAST PACIFIC RISE [J].
CRAIG, H ;
CLARKE, WB ;
BEG, MA .
EARTH AND PLANETARY SCIENCE LETTERS, 1975, 26 (02) :125-132
[10]   SLAB PENETRATION INTO THE LOWER MANTLE [J].
CREAGER, KC ;
JORDAN, TH .
JOURNAL OF GEOPHYSICAL RESEARCH, 1984, 89 (NB5) :3031-3049