华北燕山中—新元古代震积岩系列及其地震节律
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摘要
在燕山北缘河北平泉地区中、上元古界中,鉴别出一系列震积岩。主要类型有脆性型、塑性型、液化型及复合型四种。提出了啸积岩与风暴岩的鉴别标志,指出鲍马序列模式的真正拥有者是啸积岩与风暴岩,而非典型的半深海浊积岩。根据其在纵向上出现的类型和频率,划分出10个地震活跃期,其地震节律为60~80Ma,这一地震节律反映了燕山裂陷槽裂陷的历程,裂陷高峰期在高于庄至雾迷山期。
A lot of seismites were found in the Mesoproterozoic and Neoproterozoic in Pingquan, Hebei. Four main types of seismitic rocks, friability, plastic, liquefacient and multiplex, were recognized. Discriminating marks between tsunamigenic rocks and tempestite were put forward. The Bouma sequence, which may be established in tsunamigenic rocks and tempestite, is not of bathyal turbidite. According to the horizon and frequency of seismites, ten seismitic active periods can be divided. The cycle rhythm of each period was 60-80 Ma, which reflects the regularity of faulting in the northern margin of the Yanshan aulacogen.
引文
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     切片,×3,河北平泉,西水泉村,雾迷山组下部。
    9. 纹层状灰岩被震碎,形成长条状砾屑,砾屑放射状分布,上部砾屑间有碟状层理,标本切片,×2,河北平泉,小哈巴气村,高于庄组一段。
    10. 灰岩砾屑脆性、塑性两种变形,岩石发育有泄水脉,标本切片,×2,河北平泉,小哈巴气村,高于庄组二段。
    11. 薄层灰岩层间震起,期间被含砾屑的液化物充填,下部有塑性变形,标本切片,×2,河北平泉,小哈巴气村,高于庄组二段。

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