STRESS OBSERVATIONS AND DRIVING FORCE MODELS FOR THE SOUTH-AMERICAN PLATE

被引:36
作者
STEFANICK, M [1 ]
JURDY, DM [1 ]
机构
[1] NORTHWESTERN UNIV, DEPT GEOL SCI, EVANSTON, IL 60208 USA
关键词
D O I
10.1029/91JB01798
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
Stress observations are compared to predictions of driving force models for the South American plate. Stress observations have the potential to give detailed information about the forces driving the plates, in that sets of forces with the same net torque can produce quite different stress patterns. For a two-dimensional (vertical section) model of a plate there am three conditions for dynamical equilibrium: the net forces and the net torque about any point must all be zero. These conditions are used to estimate the magnitudes of forces as a function of age, with ridge push and slab pull as active forces, and plate drag and slab resistance as passive forces. The results am consistent with earlier published models, and indicate that the primary balance for an oceanic plate is between slab pull and the resisting drag forces. We generalize the model for the possible forces driving the South American plate and compare with observed stress measurements and kinematics. The South American plate has a small slab pull component, amounting to about one-fifth the ridge push force, with the other components reasonably isolated geographically, Thus, the plate balance is largely between ridge push and plate drag. This gives an opportunity of resolving the effects of trench suction or collision at the subduction zones. Most remarkable is the nearly uniform E-W orientation of the regional stress field. -SH(max) directions, which is extensional in the high Andes; a second feature is the N-S orientations in the Amazon basin. The two-dimensional, horizontal stress patterns am compared for successive models of combinations of driving forces. Models with ridge push, slab pull at the Scotia and Caribbean arcs, and trench suction near the west coast, balanced by plate drag, produce similar stress patterns to those observed. The magnitude of a possible trench suction force is estimated using a model with an eddy between the Nazca slab and the overlying South American plate.
引用
收藏
页码:11905 / 11913
页数:9
相关论文
共 24 条
[1]  
ASSUMPCAO M, 1992, J GEOPHYS RES, V97
[2]   PLATE MOTIONS, BOUNDARY FORCES, AND HORIZONTAL TEMPERATURE-GRADIENTS - IMPLICATIONS FOR THE DRIVING MECHANISM [J].
CARLSON, RL .
TECTONOPHYSICS, 1983, 99 (2-4) :149-164
[3]  
CARLSON RL, 1983, GEOPHYS RES LETT, V10, P987
[4]   THE DRIVING MECHANISM OF PLATE-TECTONICS - RELATION TO AGE OF THE LITHOSPHERE AT TRENCHES [J].
CARLSON, RL ;
HILDE, TWC ;
UYEDA, S .
GEOPHYSICAL RESEARCH LETTERS, 1983, 10 (04) :297-300
[5]   EVALUATION OF FORCES THAT DRIVE PLATES [J].
CHAPPLE, WM ;
TULLIS, TE .
JOURNAL OF GEOPHYSICAL RESEARCH, 1977, 82 (14) :1967-1984
[6]   PLATE KINEMATICS - AMERICAS, EAST-AFRICA, AND REST OF WORLD [J].
CHASE, CG .
EARTH AND PLANETARY SCIENCE LETTERS, 1978, 37 (03) :355-368
[7]   STRESS IN THE INDO-AUSTRALIAN PLATE [J].
CLOETINGH, S ;
WORTEL, R .
TECTONOPHYSICS, 1986, 132 (1-3) :49-67
[8]   SEA-FLOOR SPREADING AS THERMAL CONVECTION [J].
ELSASSER, WM .
JOURNAL OF GEOPHYSICAL RESEARCH, 1971, 76 (05) :1101-+
[9]   RELATIVE IMPORTANCE OF DRIVING FORCES OF PLATE MOTION [J].
FORSYTH, D ;
UYEDA, S .
GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1975, 43 (01) :163-200
[10]   CURRENT PLATE VELOCITIES RELATIVE TO THE HOTSPOTS INCORPORATING THE NUVEL-1 GLOBAL PLATE MOTION MODEL [J].
GRIPP, AE ;
GORDON, RG .
GEOPHYSICAL RESEARCH LETTERS, 1990, 17 (08) :1109-1112