泰国三塔断裂活动性及其板缘动力学意义  

The Activity and the Plate Margin Dynamic Significance of Three-pagoda Fault in Thailand

作　　者：张建国[1] 乔森[1] 周瑞琦[1] 胡耀雄[1] Supawan Klaipongpan Wanchai Silpon 

机构地区：[1]云南省地震局,昆明650041 [2]泰国产电机构,泰国曼谷11130

出　　处：《地震研究》2003年第1期6-13,共8页Journal of Seismological Research

摘　　要：通过对位于印度板块与欧亚板块碰撞带缅甸弧附近三塔断裂带活动性的野外考察研究 ,探讨了位于缅甸弧东侧的滇缅泰板缘地区现代构造与地震活动动力来源和空间不均匀性。指出印度板块与欧亚板块沿兴都库什弧的正面碰撞和青藏高原隆起导致的侧向挤出作用对滇缅泰板缘地区现代构造与地震活动的影响可能大于印度板块与欧亚板块沿缅甸弧的碰撞对上述地区的影响。Based on the field survey and comprehensive studies on Three-pagoda Fault developed near by collision belt between Indian Plate and Eurasia Plate in Myanmar, the spatial heterogenety and dynamic source of recent tectonic and seismic activities in Yunnan, Myanmar and Thailand areas are discussed. It seems that the influence from collision between Indian Plate and Eurasia Plate along western Himalayan Belt accompanying with the uplifting of Tibetan Plateau is more than that from collision between Indian Plate and Eurasia Plate along Myanmar Arc Belt.

关 键 词：泰国 区域构造 断裂活动 板缘动力学 地震活动 

分 类 号：P315.5[天文地球—地震学]