地学前缘
地學前緣
지학전연
2001年
2期
253-258
,共6页
曾小苹%刘正彦%林云芳%王吉易%续春荣
曾小蘋%劉正彥%林雲芳%王吉易%續春榮
증소평%류정언%림운방%왕길역%속춘영
幔羽现象%地震磁流体效应%核幔边界%平面电流模型%电离层电流体系
幔羽現象%地震磁流體效應%覈幔邊界%平麵電流模型%電離層電流體繫
만우현상%지진자류체효응%핵만변계%평면전류모형%전리층전류체계
综合分析了20世纪70年代以来发生在中国的14个强震前地磁和地下流体参量动态图像的时空演化特征,发现强震前这些参量均呈现十分明显的异常图形。这些图像十分复杂,且随时间不断变化,并与孕震过程有某种时空规律性联系。90年代地学家通过地震资料分析发现了幔羽现象。笔者设想核幔边界的幔羽磁流体物质上涌是地震电磁流体效应的一种可能成因。幔羽中的流体物质螺旋上涌至地壳的底部,并形成“蘑菇云”。流体在地壳中扩展或挤压,形成异常电流,可将其看作在孕震区地下10~20 km深处有一等效平面电流。再考虑到近地表的电磁环境——电离层电流体系的局部异常,计算了一个地下和电离层组成的等效平面电流模型在地面产生的磁场分布,结果与强震前地球磁场的零等变型异常动态图像较吻合。
綜閤分析瞭20世紀70年代以來髮生在中國的14箇彊震前地磁和地下流體參量動態圖像的時空縯化特徵,髮現彊震前這些參量均呈現十分明顯的異常圖形。這些圖像十分複雜,且隨時間不斷變化,併與孕震過程有某種時空規律性聯繫。90年代地學傢通過地震資料分析髮現瞭幔羽現象。筆者設想覈幔邊界的幔羽磁流體物質上湧是地震電磁流體效應的一種可能成因。幔羽中的流體物質螺鏇上湧至地殼的底部,併形成“蘑菇雲”。流體在地殼中擴展或擠壓,形成異常電流,可將其看作在孕震區地下10~20 km深處有一等效平麵電流。再攷慮到近地錶的電磁環境——電離層電流體繫的跼部異常,計算瞭一箇地下和電離層組成的等效平麵電流模型在地麵產生的磁場分佈,結果與彊震前地毬磁場的零等變型異常動態圖像較吻閤。
종합분석료20세기70년대이래발생재중국적14개강진전지자화지하류체삼량동태도상적시공연화특정,발현강진전저사삼량균정현십분명현적이상도형。저사도상십분복잡,차수시간불단변화,병여잉진과정유모충시공규률성련계。90년대지학가통과지진자료분석발현료만우현상。필자설상핵만변계적만우자류체물질상용시지진전자류체효응적일충가능성인。만우중적류체물질라선상용지지각적저부,병형성“마고운”。류체재지각중확전혹제압,형성이상전류,가장기간작재잉진구지하10~20 km심처유일등효평면전류。재고필도근지표적전자배경——전리층전류체계적국부이상,계산료일개지하화전리층조성적등효평면전류모형재지면산생적자장분포,결과여강진전지구자장적령등변형이상동태도상교문합。
From synthesizing the spatial and temporal pattern of anomalous dynamic images for the parameters of geomagnetic field and underground fluid for 14 strong earthquake cases occurred in China since 1970,the authors found that those parameters reveal obvious anomalous images which are very complex and changeable,and bear a regular relation with seismogenic process.In the 1990’s geo-scientists, through the processing of seismic data, discovered the phenomenon of mantle plumes at the core-mantle boundary. The authors ,from the above results and the mantle plume phenomenon, put forward that the surging-up of hydromagnetic mass at the core-mantle boundary leads to seismo-hydromagnetic effect possibly.It is imagined that the fluid mass in the conductive mantle plumes gush up spirally to the lower part of the crust and from the mushroom cloud. Then, the fluid expanded or compressed in the crust. So, there is an equivalent planar current at a depth of between 10 and 20 km in the seismogenic region.Taking into consideration of the local anomaly of the ionospheric current system—the nearest electromagnetic environment—to the earth surface, the distribution of magnetic field by a planar current model in the seismogenic region has been calculated which coincided to a certain degree with the dynamic image of zero isoporic geomagnetic field prior to strong earthquakes.