闫振,刘建波

• 1:北京大学地球与空间科学学院

摘要(Abstract)：

国外很多学者对灰泥丘的形成机制和时空演化等问题进行了讨论,但我国对这些问题的研究程度较低。目前灰泥丘的研究中仍存在一些问题,如灰泥的无机成因和微生物成因争论、客观分类方法的缺乏以及灰泥丘时空分布的研究精度低等。灰泥丘是以灰泥为主要成分的、正凸起的碳酸盐岩建造,可含有碳酸盐颗粒和平底晶洞构造等,但不具有格架构造。根据灰泥丘的成分分类方法,灰泥丘被分为4种类型,分别为生物碎屑灰泥丘、微生物灰泥丘、生物碎屑—微生物灰泥丘和纯灰泥丘。石炭纪—二叠纪灰泥丘的时空分布具有规律性,表现为石炭纪晚杜内期到早维宪期的Waulsortian丘或似Waulsortian丘、晚维宪期到谢尔普霍夫期的生物碎屑—微生物灰泥丘和石炭纪巴什基尔期到二叠纪萨克马尔期的藻灰泥丘。异地来源的灰泥通过无机堆积等物理作用形成正地形;微生物在灰泥丘的形成过程中不仅产生大量灰泥,而且起到重要的粘结巩固作用。

关键词(KeyWords)： 岩石地层;灰泥丘;分类方法;形成机制;灰泥来源;时空分布;控制因素;石炭纪;二叠纪;内蒙古

Abstract:

Keywords:

基金项目(Foundation): 国家自然科学基金(No.41272035,41221001,41290260)支持;; IGCP591项目“早、中古生代生物事件”的阶段成果

作者(Author): 闫振,刘建波

DOI: 10.19839/j.cnki.dcxzz.2016.04.011

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