东营凹陷牛38井始新统沙河街组三段米氏旋回的地层响应STRATIGRAPHIC RESPONSE TO THE MILANKOVITCH CYCLES IN THE MEMBER 3 OF SHAHEJIE FORMATION OF WELL NIU 38 IN THE DONGYING DEPRESSION
边雪梅,张海峰,姚益民,何青芳
摘要(Abstract):
地球围绕太阳的轨道要素周期性变化引起气候旋回变化,进而影响到地质历史中沉积物及生物面貌的旋回变化。牛38井始新统沙河街组三段旋回地层学研究表明,沉积物和古生物对404.8ka的天文偏心率旋回具有明显的响应特征。在一个偏心率旋回之内,随着地球围绕太阳公转轨道位置的变化,气候由热变冷再变热,古生物属种数量、沉积物粒度出现相应的的旋回变化。若以404.8ka偏心率旋回为单位来划分高频层序,可以保证所划分的地层具有异旋回性和严格的等时性。
关键词(KeyWords): 高频层序;米氏旋回;沙河街组;始新统;东营凹陷;山东
基金项目(Foundation): 国家自然科学主任基金项目(No40542007)的部分研究成果
作者(Author): 边雪梅,张海峰,姚益民,何青芳
DOI: 10.19839/j.cnki.dcxzz.2007.s2.009
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