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中国地层表及说明书的特点与主要进展

王泽九 黄枝高 姚建新 马秀兰

地球学报Issue(3):271-276,6.
地球学报Issue(3):271-276,6.DOI:10.3975/cagsb.2014.03.01

中国地层表及说明书的特点与主要进展

Characteristics and Main Progress of The Stratigraphic Chart of China and Directions

王泽九 1黄枝高 2姚建新 2马秀兰1

作者信息

  • 1. 中国地质科学院,北京 100037
  • 2. 中国地质科学院地质研究所,北京 100037
  • 折叠

摘要

Abstract

Under the leadership of National Commission on Stratigraphy of China, The Stratigraphic Chart of China and Directions were compiled by Chinese stratigraphers. The exact correlation between international chronostratigraphy and Chinese chronostratigraphy is established in The stratigraphic Chart of China. The Stratigraphic Chart of China fully reflects the distributive status of lithostratigraphy, the characteristics of geological ages, the biostratigraphic sequence, the magnetostratigraphy, the geological events and the eustatic sea level change during every geological period. According to recent research, some schemes of stratigraphic division of Mesoproterozoic-Neoproterozoic, Cambrian, and Jurassic-Cretaceous were revised. In order to avoid the repetition of names between stage and formation, the compilers adjusted some stage names of Mesozoic and Paleozoic. The Stratigraphic Chart of China is possessed of important scientific significance and practical value for us to understand the development of Chinese stratigraphy, correlate stratigraphy between China and foreign countries, and unfold scientific research, geological education and geological survey. Therefore, The Stratigraphic Chart of China was well received and highly praised by the 34th International Geological Congress and 4th National Stratigraphic Congress. A part of achievements has been widely applied to geological survey and compilation of regional geological records, with good social benefit achieved.

关键词

中国/地层表/特点/主要进展

Key words

China/stratigraphic chart/characteristics/main progress

分类

社会科学

引用本文复制引用

王泽九,黄枝高,姚建新,马秀兰..中国地层表及说明书的特点与主要进展[J].地球学报,2014,(3):271-276,6.

基金项目

本文由中国地质调查局地质调查项目“全国多重地层表及说明书编制”(编号:1212010811057)资助。获中国地质科学院2013年度十大科技进展第一名。 (编号:1212010811057)

地球学报

OA北大核心CSCDCSTPCD

1006-3021

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