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王之前:泥丘岩体的地震地质解释,《石油地球物理勘探》,23(1)1988:83～89泥丘是莺歌海盆地西部凹陷发育的特殊岩体。自渐新世至上新世该区一直处于泥(页)岩发育区,巨厚的大套泥质成分经上新世以来的快速沉降的负载下压,使该套地层上下界面附近孔渗封阻,形成高压地层,从而导致泥丘出现。泥丘分为膨胀型丘体和刺穿侵入型丘体。文中通过对泥丘岩体的地质、地球物理特征分析及其形成机理与识别方法的讨论,进一步证实了该区泥丘的存在。
Wang Qianqian: Seismic Geological Interpretation of Mud Chiroflora, Petroleum Geophysical Prospecting, 23 (1) 1988: 83-89 Mud mound is a special rock mass developed in the western depression of the Yinggehai Basin. Since the Oligocene to the Pliocene, the area has been in the mud development area, and the huge thick muddy component under rapid subsidence load since the Pliocene underwent the seepage sealing of the upper and lower interfaces Resistance, the formation of high pressure formations, resulting in mud mound. Mud is divided into swelling mound and piercing invasive mound. Through the discussion of the geology and geophysical characteristics of mud mound body and its formation mechanism and identification method, the existence of mud mound in this area is further confirmed.