地震地热说原理与应用
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摘要
从地震与火山资料出发,定义了地震柱的概念,全球划分24个地震柱并逐个研究。发现了地幔深部能量自下而上逐层驱动的稳定通道,揭示了浅源地震与中深源地震的差异性、壳内地震与火山的同一性、本尼奥夫剖面的独立性、地震柱活动的间歇性、地震柱的衰变性等自然现象,探讨了地震柱的成因,构成了M型的热机带。同时,对全球GPS观测资料与大洋中脊带的继承性运动和脊轴扩张的比较研究,揭示了当前大陆漂移的优势方向,构成了W型的冷机带。两大系统呈倒扣之势并具有相位差异或许由于地球自转角速度的变更所造成,从而构成了当今地球的地貌差异。冷机带造成大陆漂移的渐变而热机带造成壳内强震和火山的灾变,形成地震地热说的两个研究体系。文中给出了地震地热说应用方面的几个例子。
Based on earthquake and volcano data,the concept of seismic cylinder was defined,and global earthquakes were not only divided into 24 seismic cylinders but studied one by one.The stable channels of the deep mantle energy driven layer-by-layer bottom-up were found.Some natural phenomena such as the difference of shallow source earthquakes and intermediate and deep-focus earthquakes,identity of earthquake and volcano,the independence of Benioff profile,the intermittent of seismic cylinder activity and the decay of seismic cylinder were revealed.The formation cause of seismic cylinder and a type M heat engine belt were also discussed.In addition,through contrast studies of the global GPS observation data,inheritance motion and ridge axis expansion of the oceanic ridge,the author revealed the current continental drift dominant directions and the W type refrigerating belt was formed.Two systems with inverted trend and phase difference may be caused by the changes of the earth rotation angular velocity,which constitute a topographic differentiation.Refrigerating belt caused gradual change of continental drift and heat engine belt caused shell disaster of earthquake and volcano,which formed two research systems of Seismo-geothermics.Some application examples of the Seismo-geothermics were shown also in this paper.
Based on earthquake and volcano data,the concept of seismic cylinder was defined,and global earthquakes were not only divided into 24 seismic cylinders but studied one by one.The stable channels of the deep mantle energy driven layer-by-layer bottom-up were found.Some natural phenomena such as the difference of shallow source earthquakes and intermediate and deep-focus earthquakes,identity of earthquake and volcano,the independence of Benioff profile,the intermittent of seismic cylinder activity and the decay of seismic cylinder were revealed.The formation cause of seismic cylinder and a type M heat engine belt were also discussed.In addition,through contrast studies of the global GPS observation data,inheritance motion and ridge axis expansion of the oceanic ridge,the author revealed the current continental drift dominant directions and the W type refrigerating belt was formed.Two systems with inverted trend and phase difference may be caused by the changes of the earth rotation angular velocity,which constitute a topographic differentiation.Refrigerating belt caused gradual change of continental drift and heat engine belt caused shell disaster of earthquake and volcano,which formed two research systems of Seismo-geothermics.Some application examples of the Seismo-geothermics were shown also in this paper.
引文
陈立军.全球地震震源深度与地震地幔柱的研究.湖南地震(内刊),2011.
陈立军.全球地震、火山和地幔柱的比较研究,中国地震局老专家科研基金课题论文摘编(2007～2009).
陈立军.试论地震预测与火山预测的同一性,地震预报与历史地震专业委员会联合学术交流会摘要集,2011,83.
陈立军,陈晓逢.美国西海岸地震预测方法初探.湖南地震,2012(34).
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[3]刘嘉麒.中国火山[M].北京:科学出版社,1999.
[4]Davies G F.地幔柱存在的依据[J].科学通报,2005,(50)17:1801-1813.
[5]Foulger G R.地幔柱:为什么现在怀疑?[J].科学通报,2005,(50)17:1814-1819.
[6]牛耀龄.关于地幔柱大辩论[J].科学通报,2005,(50)17:1797-1800.
[7]Peacock S M.Thermal Structure and Metamorphic Evolution of Subducting Slabs,Peacock 2000-Subduction Factory TEI,p.1-9.
[8]金性春.板块构造学基础[M].上海:上海科学技术出版社,1984.
[9]Brun J P,Oncken O,Weissert H,et al.Subduction Zone Geodynamics[M].Roma:Springer-Verlag Berlin Heidelberg.2009,50-55.
[10]Guoming Jiang,Dapeng Zhao,Guibin Zhang.Seismic tomography of the Paci?c slab edge under Kamchatka[J].Tectono-physics,2009,465:190-203.
[11]赵大鹏,雷建设,唐荣余.中国东北长白山火山的起源:地震层析成像证据[J].科学通报,2004,(49)14:1439-1446.
[12]Foulger G R,Pritchard M J,Julian,et al.Seismic tomography shows that upwelling beneath Icelandis con?ned to the uppermantle[J].Geophys.J.Int.2001,146,504-530.
[13]Dapeng Zhao.Multiscale seismic tomography and mantle dynamics.Gondwana Research 15,2009,297-323.
[14]国家地震局《深部物探成果》编写组.中国地壳上地幔地球物理探测成果[M].北京:地震出版社,1986.
[15]赵苏民,高宝珠,黎雪梅,等.沧东断裂(天津段)特征及导水导热性质分析[J].地质调查与研究,2007,(2):43-49.
[16]白登海,腾吉文,马晓冰,等.大地电磁观测揭示青藏高原东部存在两条地壳物质流[J].中国基础科学.研究进展,2011,
[17]John Watson.Where Is It?[EB/OL][1997-06-24]http://pubs.usgs.gov/gip/earthq3/where.html.
[18]李四光原著,《中国地质学》扩编委员会编著.中国地质学(扩编版)[M].北京:地质出版社.1999.
[19]刘雷,杜建国,易丽.亚稳态橄榄石相变与深源地震研究进展[J].地震,(27)3,2007,41-49.
[20]赵文津.大陆漂移,板块构造,地质力学[J].地球学报,2009,(30)6:717-731.
陈立军.全球地震、火山和地幔柱的比较研究,中国地震局老专家科研基金课题论文摘编(2007～2009).
陈立军.试论地震预测与火山预测的同一性,地震预报与历史地震专业委员会联合学术交流会摘要集,2011,83.
陈立军,陈晓逢.美国西海岸地震预测方法初探.湖南地震,2012(34).
[1]胡明,廖太平.构造地质学[M].石油工业出版社,2007,156.
[2]陈立军.中国地震震源深度与强震活动状态研究[J].地震地质.2000,(22)4:360-370.
[3]刘嘉麒.中国火山[M].北京:科学出版社,1999.
[4]Davies G F.地幔柱存在的依据[J].科学通报,2005,(50)17:1801-1813.
[5]Foulger G R.地幔柱:为什么现在怀疑?[J].科学通报,2005,(50)17:1814-1819.
[6]牛耀龄.关于地幔柱大辩论[J].科学通报,2005,(50)17:1797-1800.
[7]Peacock S M.Thermal Structure and Metamorphic Evolution of Subducting Slabs,Peacock 2000-Subduction Factory TEI,p.1-9.
[8]金性春.板块构造学基础[M].上海:上海科学技术出版社,1984.
[9]Brun J P,Oncken O,Weissert H,et al.Subduction Zone Geodynamics[M].Roma:Springer-Verlag Berlin Heidelberg.2009,50-55.
[10]Guoming Jiang,Dapeng Zhao,Guibin Zhang.Seismic tomography of the Paci?c slab edge under Kamchatka[J].Tectono-physics,2009,465:190-203.
[11]赵大鹏,雷建设,唐荣余.中国东北长白山火山的起源:地震层析成像证据[J].科学通报,2004,(49)14:1439-1446.
[12]Foulger G R,Pritchard M J,Julian,et al.Seismic tomography shows that upwelling beneath Icelandis con?ned to the uppermantle[J].Geophys.J.Int.2001,146,504-530.
[13]Dapeng Zhao.Multiscale seismic tomography and mantle dynamics.Gondwana Research 15,2009,297-323.
[14]国家地震局《深部物探成果》编写组.中国地壳上地幔地球物理探测成果[M].北京:地震出版社,1986.
[15]赵苏民,高宝珠,黎雪梅,等.沧东断裂(天津段)特征及导水导热性质分析[J].地质调查与研究,2007,(2):43-49.
[16]白登海,腾吉文,马晓冰,等.大地电磁观测揭示青藏高原东部存在两条地壳物质流[J].中国基础科学.研究进展,2011,
[17]John Watson.Where Is It?[EB/OL][1997-06-24]http://pubs.usgs.gov/gip/earthq3/where.html.
[18]李四光原著,《中国地质学》扩编委员会编著.中国地质学(扩编版)[M].北京:地质出版社.1999.
[19]刘雷,杜建国,易丽.亚稳态橄榄石相变与深源地震研究进展[J].地震,(27)3,2007,41-49.
[20]赵文津.大陆漂移,板块构造,地质力学[J].地球学报,2009,(30)6:717-731.
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