Future directions in subduction modeling

被引:206
作者
Gerya, Taras [1 ]
机构
[1] Swiss Fed Inst Technol, Geophys Fluid Dynam Grp, Inst Geophys, Dept Earth Sci, CH-8092 Zurich, Switzerland
关键词
Numerical modeling; Plate tectonics; Subduction zones; Slab dynamics; Mantle convection; Magmatic arcs; Subduction initiation and termination; SPONTANEOUS SLAB BREAKOFF; CONVERGENT PLATE MARGINS; SMALL-SCALE CONVECTION; MANTLE WEDGE PLUMES; SAN-JUAN COMPLEX; CONTINENTAL-CRUST; ISLAND-ARC; ULTRAHIGH-PRESSURE; THERMOMECHANICAL MODEL; NUMERICAL-SIMULATION;
D O I
10.1016/j.jog.2011.06.005
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
During the last four decades, subduction remained one of the most challenging and captivating geodynamic processes investigated with numerical techniques. While significant progress has been made toward deciphering the diverse array of subduction zone observations within the context of modeled physical processes, numerous questions remain regarding multiple aspects of subduction zone dynamics. A review of recent numerical studies highlights a number of open topics that subduction modeling can provide significant insight into in the future: 1. Resolving the controversy of subduction initiation. 2. Constraining robust high-resolution models of terrestrial plate tectonics. 3. Understanding deep slab processes in the mantle. 4. Constraining crustal growth and differentiation in magmatic arcs. 5. Modeling of fluid and melt transport in subduction zones. 6. Deciphering evolution of high- and ultrahigh-pressure rock complexes. 7. Developing geochemical-thermo-mechanical models of subduction. 8. Coupling of subduction models with volcanic and seismic risk assessment. 9. Understanding the onset of plate tectonics on Earth. Progress in subduction modeling will require strong input from other disciplines (rheology, phase petrology, seismic tomography, geochemistry, numerical analysis, etc.). Indeed, due to the intrinsic complexity of terrestrial subduction processes, the role of geodynamic modeling will inevitably grow and provide an integrative basis for conducting quantitative cross-disciplinary subduction studies combining natural observations, laboratory experiments and modeling. (C) 2011 Elsevier Ltd. All rights reserved.
引用
收藏
页码:344 / 378
页数:35
相关论文
共 260 条
[1]   P-T path for ultrahigh-pressure garnet ultramafic rocks of the Cuaba Gneiss, Rio San Juan complex, Dominican Republic [J].
Abbott, Richard N., Jr. ;
Draper, Grenville ;
Broman, Bonnie N. .
INTERNATIONAL GEOLOGY REVIEW, 2006, 48 (09) :778-790
[2]   SUBDUCTION AND EDUCTION OF CONTINENTAL-CRUST - MAJOR MECHANISMS DURING CONTINENT-CONTINENT COLLISION AND OROGENIC EXTENSIONAL COLLAPSE, A MODEL BASED ON THE SOUTH NORWEGIAN CALEDONIDES [J].
ANDERSEN, TB ;
JAMTVEIT, B ;
DEWEY, JF ;
SWENSSON, E .
TERRA NOVA, 1991, 3 (03) :303-310
[3]   Rheologic controls on the dynamics of slab detachment [J].
Andrews, Erin R. ;
Billen, Magali I. .
TECTONOPHYSICS, 2009, 464 (1-4) :60-69
[4]  
[Anonymous], GEOLOGICAL SOC AM SP
[5]   Overriding plate thinning in subduction zones: Localized convection induced by slab dehydration [J].
Arcay, D ;
Doin, MP ;
Tric, E ;
Bousquet, R ;
de Capitani, C .
GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS, 2006, 7
[6]   Numerical simulations of subduction zones - Effect of slab dehydration on the mantle wedge dynamics [J].
Arcay, D ;
Tric, E ;
Doin, MP .
PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 2005, 149 (1-2) :133-153
[7]   Back-arc strain in subduction zones: Statistical observations versus numerical modeling [J].
Arcay, D. ;
Lallemand, S. ;
Doin, M. -P. .
GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS, 2008, 9
[8]   High-resolution numerical modeling of stress distribution in visco-elasto-plastic subducting slabs [J].
Babeyko, A. Y. ;
Sobolev, S. V. .
LITHOS, 2008, 103 (1-2) :205-216
[9]   DESCENT OF LITHOSPHERE BENEATH NEW HEBRIDES, TONGA-FIJI AND NEW ZEALAND - EVIDENCE FOR DETACHED SLABS [J].
BARAZANGI, M ;
ISACKS, BL ;
OLIVER, J ;
DUBOIS, J ;
PASCAL, G .
NATURE, 1973, 242 (5393) :98-101
[10]  
Baumann C, 2010, GEOL SOC SPEC PUBL, V332, P99, DOI 10.1144/SP332.7