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全息地层学原理与方法综述
引用本文:吴智勇,姜衍文.全息地层学原理与方法综述[J].地质论评,1995,41(5):426-431.
作者姓名:吴智勇  姜衍文
作者单位:江汉石油学院 湖北荆沙 (吴智勇),江汉石油学院 湖北荆沙(姜衍文)
摘    要:全息地层学是以全球旋回地层学和高分辨率事件地层学为基础,综合生物地层学、磁性地层学、化学层学以及构造地层学等地层学各个分支的研究结果,以崭新的思路,全方位地开发和提取出沉积记录中所蕴涵的各类地层学信息,从而以极高的时间精度划分对比地层的综合性地层学。

关 键 词:全息地层学  旋回沉积层  事件沉积层  地层

HOLOSTRATIGRAPHY AND ITS RESEARCHING APPROACH
Wu Zhiyong and Jiang Yanwen.HOLOSTRATIGRAPHY AND ITS RESEARCHING APPROACH[J].Geological Review,1995,41(5):426-431.
Authors:Wu Zhiyong and Jiang Yanwen
Abstract:Holostratigraphy is a comprehensive stratigraphy based on the global cyclostratigraphy and high resolution event stratigraphy, combined with biostratigraphy, magnetostratigraphy, chemostratigraphy, and other branchs of stratigraphy. The holostratigraphy suggests that it should be done to develop and extract the all of the information inherent in strata so as to devide and correlate the strata in the highest resolution. The methods, the objects and the fundament of the holostratigraphy are systematically dealt with.
Keywords:holostratigraphy  cycle deposit  event deposit  high resolution correlation
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