对莲花山断裂带已从不同的角度进行了广泛的研究。由于其西南端的活动性渐趋和缓,并被南海所淹没,故不为人们所注意。作者近年来对海丰、深圳等地进行地震基本烈度研究时发现,莲花山断裂带西南段之新构造活动并不比其它各段低落,只是表现形式不一,其活动性主要体现在地震比较活跃,是新构造活动上值得重视的地区。 The Lianhua Mountain fault zone has been studied extensively from different angles. Due to its activity on the southwestern end of the island has gradually slowed down and was inundated by the South China Sea, it is not for people’s attention. In recent years, the authors study the basic intensity of the earthquake in Haifeng, Shenzhen and other places. It is found that the new tectonic activity in the southwestern segment of the Lianhuashan fault zone is not lower than that in other segments, but its forms are different. Its activity is mainly reflected in the active earthquakes , Is the new structure of activities worthy of attention to the area.