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泉州——汕头地震带是华南(除台湾省外)地震最频繁的地段,自九世纪有地震记载以来,多次发生破坏性地震,历来为南方地震工作者所注视。最近几年,各单位通过地震史料的发掘和整理,对该带地震活动又有不少新的发现,有些还是以往地震目录中遗漏的大震。本文仅对1906年3月28日泉州-厦门海外大震及一些有关问题提出初步报导,以便同志们在研究该带地震活动性时引起必要的注意。
The Quanzhou-Shantou seismic belt is the most frequent earthquake in southern China (except Taiwan Province). Since the earthquake was recorded in the 9th century, many destructive earthquakes have occurred and it has always been the focus of the earthquake workers in the south. In recent years, through the excavation and arrangement of historical materials, various units have found many new discoveries on the seismic activity of the belt, some of which were missed by the previous earthquake catalogs. This article gives preliminary reports only on the March 28, 1906 Quanzhou-Xiamen earthquake and some related issues so that comrades can draw the necessary attention when studying the seismicity of the belt.