大陆动力学的过去、现在和未来——理论与应用
摘要
近十年来大陆岩石圈流变学、板块下的构造和整个地幔运动、现代大陆变形动力学、大陆深俯冲动力学、"中下地壳的隧道流"、复合造山带和复合造山动力学、盆-山耦合与大陆增生、地幔物质和地幔动力学以及全球大陆科学钻探整合计划等大陆动力学研究的重要进展,表明大陆动力学是继"板块构造"之后固体地球科学发展的新的起点,建立大陆动力学新的理论体系以及为资源、能源、环境和预防地震灾害的人类需求服务,是大陆动力学发展的未来。
This paper presents an overview on advances and prospectives of continental dynamics with a special focus on the rheology of continental lithosphere.,tectonics of the entire mantle beneath plates,modern continental deformation dynamics,continental deep-subduction dynamics,channel flow in the mid-lower crust,dynamics of eomposive orogenic belts,basin-range coupling and continental accretion,mantle compositions and mantle tectonics,and global continental scientific drilling integration plans.It is concluded that the continental dynamics is a new departure following plate tectonics and it is critical necessary to establish a new theorical system of continental dynamics for satisfying the human needs for resources,energy,environmental protection,and prevention/mitigation of earthquake harzards.
This paper presents an overview on advances and prospectives of continental dynamics with a special focus on the rheology of continental lithosphere.,tectonics of the entire mantle beneath plates,modern continental deformation dynamics,continental deep-subduction dynamics,channel flow in the mid-lower crust,dynamics of eomposive orogenic belts,basin-range coupling and continental accretion,mantle compositions and mantle tectonics,and global continental scientific drilling integration plans.It is concluded that the continental dynamics is a new departure following plate tectonics and it is critical necessary to establish a new theorical system of continental dynamics for satisfying the human needs for resources,energy,environmental protection,and prevention/mitigation of earthquake harzards.
引文
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Dewey JF.2005． Orogeny can be very short.Proceeding of the National Academy of Sciences,102:15286-15293
Dickinson WR.1993． Basin geodynamics.Basin Research,5:195-196
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Gerya TV and Stockhert B.2002． Exhumation rates of high pressure metamorphic rocks in subduction channels:The effect of rheologh.Geophysical Research Letters,29． DOI:10． 1029/2001GL014307
Godin L,Gleeson TP,Searle MP,Ullrich TD and Parrish RR.2006． Locking of southward extrusion in favour of rapid crustal-scale bucking of the Greater Nepal.In:Law RD,Searle MP and Godin L (eds.).Channel flow,Ductile Extrusion and Exhumation in Continental Collision Zones.Geological Society,London,Special Publications,268:269-292
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Grujie D,Casey M,Davidson C,Hollister LS,Kundig R,Pavlis T and Sehmid S.1996． Ductile extrusion of the Higher Himalayan Crystalline in Bhutan:Evidence from quartz micro-fabrics.Teetonophysics,260:21-43
Grujie D,Hollister L and Parish R.2002． Himalayan metamorphic sequence as an orogenic channel:Insight from Bhutan.Earth and Planetary Science Letters,198:177-191
Hacker BR,Simon MP,Geoffrey AA and Stephen DH.2003． Subduetion factory:2． Are intermediate-depth earthquakes in subducting slabs linked to metamorphic dehydration reactions? Journal of Geophysical Research,108(B1) .DOI:10． 1029/2001JB001129
Haggerty SE.1994． Superkimberlites:A geodynamie diamond window to the Earth's core.Earth and Planetary Science Letters,122 (1-2) :57-69
Harrision TM.2006． Did the Himalayan Crystallines extrude partially molten from beneath the Tibetan Plateau? In:Law RD,Searle MP and Godin L (eds.).Channel Flow,Ductile Extrusion and Exhumation in Continental Collision Zones.Geological Society,London,Special Publications,268:237-254
Hatcher RD and Mersehat AJ.2006． The Appalachian Inner Piedmont:An exhumed strike-parallel,teetonieally forced orogenic channel In:Law RD,Searle MP and Godin L (eds.).Channel Flow,Ductile Extrusion and Exhumation in Continental Collision Zones.Geological Society,London,Special Publications,268:517-541
Haughton PDW,Todd SP and Morton AC.1991． Sedimentary provenance studies.Geological Society,London,Special Publications,57:1-11
Hilley GE,Burgmann R,Zhang PZ and Molnar P.2005． Bayesian inference of plastosphere viscosities near the Kunlun Fault,northern Tibet.Geophysical Research Letters,32,L01302． DOI:01310． 01029/02004GL021658
Hollister LS and Grujic D.2006． Puled channel flow in Bhutan.In:Law RD,Searle MP and Godin L (eds.).Channel flow,Ductile Extrusion and Exhumation in Continental Collision Zones.Geological Society,London,Special Publications,268:415-423
Hyndman RD,Currie CA and Mazzotti SP.2005． Subduction zone backarcs,mobile belts,and orogenic heat.GSA Today,15 (2) .DOI:10． 1130/1052-5173(2005) 015
Ingersoll RV and Busby CJ.1995． Tectonics of Sedimentary Basins.Cambridge:Blackwell Science,1-51
Jamieson RA,Beaumont C,Medvedev S and Nguyen MH.2004． Crustal channel flows:2． Numrical models with implications for metamorphism in the Himalayan-Tibetan Orogen.Journal of Geophysical Research,109． DOI:10． 1029/2003JB002811
Jamieson RA,Beaumont C,Nguyen MH and Grujic D.2006． Provenace of the Greater Himalayan Sequence and associated rocks:Predictions of channel flow models.In:Law RD,Searle MP and Godin,L (eds.).Channel flow,Ductile Extrusion and Exhumation in Continental Collisian Zones.Geological Society,London,Special Publications,268:165-182
Jessup MJ,Law RD,Searle MP and Hubbard MS.2006． Structural evolution and vorticity of flow during extrusion and exhumation of the Greater Himalayan Slab,Mount Everest massif,Tibet/Nepal:Implications for orogen-scale flow partitioning.In:Law RD,Searle MP and Godin L (eds.).Channel flow,Ductile Extrusion and Exhumation in Continental Collision Zones.Geological Society,London,Special Publications,268:379-414
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