吕梁山地区新近纪晚期地层研究进展NEW ADVANCES IN THE STUDY OF LATE NEOGENE STRATIGRAPHY IN THE LLIANG MOUNTAIN
李建星,岳乐平,徐永,孙勃,孙蕗,王晓勇
摘要(Abstract):
通过对吕梁山西部保德和柳林两个典型剖面的研究,认为山西柳林卫家洼保德组剖面结构与保德剖面相同,完全可以对比。保德组下部的砂砾石确为水成堆积无疑,但是上部的棕红色黏土与棕黄色的钙质结核层越来越被广大学者认为是风尘堆积,中部则为下部水成堆积物与上部红黏土与钙质结核的过渡地段。《中国地层指南及中国地层指南说明书》规定:组的含义在于岩性、岩相和变质程度的一致性,除去变质程度不说,保德组下部水成堆积物和上部风尘堆积根本不是同一相环境所能包含的岩石组合,因此不能用一个组来定义,应予解体。保德组下部的水成堆积物划为芦子沟组,相当于初始定义的"芦子沟系"或"芦子沟砾岩";保德组上部风尘堆积仍称之为保德组,相当于初始定义的保德红土;在这种划分下芦子沟组为不整合于前新生代基岩之上,整合伏于红黏土之下的山前冲积扇相堆积。保德组为整合于芦子沟组之上静乐组之下的所有风尘堆积。
关键词(KeyWords): 保德组;静乐组;芦子沟组;新近纪;吕梁山;柳林;保德;山西
基金项目(Foundation): 国家重点基础研究发展计划项目(No.2003CB214607);; 教育部长江学者和“油气盆地”创新团队发展计划项目(No.IRT0559);; 国家自然科学基金项目(No.40372202);; 中国科学院黄土与第四纪地质国家重点实验室开放基金项目(No.SKLLQG0511);; 中国地质调查局项目(No.20022307,1212010610313)共同资助
作者(Author): 李建星,岳乐平,徐永,孙勃,孙蕗,王晓勇
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