华北克拉通岩石圈二维P波速度结构特征——文登-阿拉善左旗深地震测深剖面结果
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摘要
利用超长观测距地震宽角反射/折射剖面探测技术,获得了近东西向横穿华北克拉通不同块体的反映地壳-上地幔岩石圈结构的不同深度、不同属性地震波震相特征数据.通过对各个块体内的地震波震相特征对比分析研究,除识别出地壳内常规的Pg波、Pci波、Pm P波和Pn波外,还清楚的对比出了岩石圈尺度的两组震相PL1和PL2波.经过一维、二维地震走时及波形拟合,获得了沿剖面长约1500 km的不同块体的壳幔二维速度结构与构造特征.结果表明:沿剖面地壳及岩石圈自东向西加厚趋势的明显,但各组地震波反、折射界面在各个块体内又显示出局部变化明显等特征.结晶基底在各个块体内变化较大,在华北凹陷盆地内最深达到7.8 km,在胶东半岛及太行吕梁地块较浅约2.0 km;莫霍界面形态整体显示出东浅西深,在鄂尔多斯块体内最深达到46 km,而在华北断陷盆地内显示隆起特征;L1界面仅在太行山以西区域显示,深度约为80 km,变化较缓.岩石圈L2界面东浅西深在75~160 km范围内变化,在太行山以西有一急剧加深趋势,形成一个陡变带.
引文
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