长江、黄河大洪水前期地球系统演变的分析

THE ANALYSIS ON THE EVOLUTION OF EARTH SYSTEM BEFORE THE FLOODS IN YANGTSE RIVER AND YELLOW RIVER

通过分析江、淮、黄、海四大河共 1 4个大洪水年的前期地震场特征 ,发现大洪水前在青藏高原东南地区、亚欧中纬地带和台湾以东洋面三处均有强地震发生。若强震出现在中印缅热点区则对应着江淮大水 ;强震出现在川青甘地区则对应着黄海河大水。引发大水的直接原因是本地区地热涡的强烈发展 ,它因刚好位于数组“同向等距地热涡族”的相交点上 ,受相干共振的结果。文中详细分析了 1 954和 1 982年两个个例。最后分析了“中印缅热点”的强热脉冲存在准半年韵律的事实。将它与大气对流边界层中的“大涡”自组织现象作了初步对比。

After analyzing the characteristics of seismic fields in the early stage of 14 flood years of Yangtse River, Huaihe River, Yellow River and Haihe River, it is found that there were earthquakes happening in southeast part of Qinghai Xizang Plateau, in mid latitude zone of Eurasia and in east part to Taiwan. When earthquake happened in the hotspot region of China, India and Burma, floods occurred in Yangtse River and Huaihe River; the earthquake in the conjunction area among Sichuan province, Qinghai province and Gansu province corresponds to the flood in Yellow River and Huaihe River. The direct cause is the strong development of geothermal vortex in the region, which located at the cross point of several “Isogonic Equidistant Geothermal Vortex Families”, it is the result of sympathetic vibration. The facts in 1954 and in 1982 were analyzed in detail as examples. It was discovered that there is a quasi half year rhythm of strong thermal pulse in the hotspot region in the conjunction of China, India and Burma. And it was compared with the self organizing phenomenon in atmospheric convective boundary layer.