吉林大学学报(地球科学版) ›› 2016, Vol. 46 ›› Issue (3): 781-797.doi: 10.13278/j.cnki.jjuese.201603114
杨海斌1,2, 田小波1, 白志明1, 张中杰1
Yang Haibin1,2, Tian Xiaobo1, Bai Zhiming1, Zhang Zhongjie1
摘要:
本文旨在厘清中生代中国东缘受泛太平洋板块俯冲作用影响下,其可能形成的地质记录的时空分布与泛太平洋板块活动的关系。前者主要从岩浆、构造、沉积盆地的时空演化等角度出发,后者的运动学参数集中在俯冲角度、速度、方向等维度。结果显示:俯冲角度、速度以及方向的改变都有可能形成与之对应的地质事件;但是中国东缘(东北、华北和华南)区域地质记录间的差异也表明,即使都可能遭受俯冲作用,由于个体特殊的构造背景,最终的结果也不尽相同。我们对于中国东缘中、新生代的这一特殊构造现象进行了讨论,得出如下结论:首先三联点力学稳定性分析结果认为,在华北和华南碰撞拼合后,中国大陆东缘可能存在TTT、TTR或者TFT的三联点,而不是简单的稳定的被动大陆边缘;另外,中国华南早、中侏罗世近东西向岩浆岩的形成可能与法拉隆板块和伊泽奈岐板块洋中脊俯冲有关;晚侏罗-早白垩世的板片后撤由NWW向的伊泽奈岐板块与太平洋板块的洋中脊扩张作用所致;而华北克拉通东部记录侏罗纪伊泽奈岐板块俯冲的证据不足,可能并没有发生板块俯冲作用,表现为板块运动与作为中国东部最为薄弱地区的郯庐断裂带的强烈耦合作用。
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