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浙江长兴煤山剖面Griesbachian期旋回地层研究
引用本文:童金南,殷鸿福.浙江长兴煤山剖面Griesbachian期旋回地层研究[J].地层学杂志,1999,23(2):130-135.
作者姓名:童金南  殷鸿福
作者单位:中国地质大学地球科学学院,湖北,武汉,430074
基金项目:国家自然科学基金重点项目
摘    要:浙江长兴煤山剖面Griesbachian期地层由一系列多级泥—灰岩层束旋回所组成,层束的结构型式和空间叠置关系是层序地层中层序和体系域识别和区分的良好标志。旋回层束中碳酸盐岩含量变化的时间序列分析表明,其形成机制与米兰柯维奇天文气候周期密切相关,从而将地层研究的分辨率提高到了万年级(104年)。

关 键 词:旋回地层学,时间序列分析,下三叠统,煤山剖面,浙江
修稿时间:1997-05-17

A Study on the Griesbachian Cyclostratigraphy of Meishan Section,Changxing,Zhejiang Province
Tong Jinnan,Yin Hongfu.A Study on the Griesbachian Cyclostratigraphy of Meishan Section,Changxing,Zhejiang Province[J].Journal of Stratigraphy,1999,23(2):130-135.
Authors:Tong Jinnan  Yin Hongfu
Abstract:The Griesbachian strata of the Meishan Section,Changxing County,Zhejiang Province,Southeast China are composed of a series of multievel cycles of the mudrock limestone bundles.The composition of the bundles and their stacking patterns are the excellent markers for distinguishing and identifying the sequence and system tracts in sequence stratigraphy.The time series analysis of the carbonate contents of the bundles shows that the formation of the bundles and the higher cycles was closely related to the astronomical Milankovitch climate cycles,so that the resolution of the studied strata is greatly improved up to the scale of 10 4 years.
Keywords:cyclostratigraphy  time series    analysis    Triassic  Meishan Section  Zhejiang  
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