中国层序地层研究现状和发展方向
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摘要
层序地层学在中国已经近 2 0年 ,通过中国地质学家的努力下 ,层序地层学的发展可以分为 :萌芽阶段 ,快速发展阶段 ,成熟发展阶段。在中国区域层序地层研究、在层序地层理论体系、层序地层与矿产控制作用、层序地层与油气勘探、高分辨层序地层和米兰柯维奇旋回及米级旋回层序地层、陆相层序地层 (包括冲积体系和沙漠体系 )、新技术、新方法在层序地层中的应用 (包括地震、测井、计算机模拟、中子技术、宇宙核素等 )、盆山转换和动力层序地层、青藏高原层序地层及造山带层序地层、成岩层序地层和化学层序地层、构造层序地层、层序地层岩相古地理编图等各个方面都有很大发展 ,取得了丰硕的成果。在中国层序地层学研究状况分析基础上 ,提出中国层序地层学应该在加强应用 ,重视基础 ,提高技术 ,发展特色等四个方面努力创新 ,为层序地层学科的发展贡献中国地质学家的力量。
Sequence stratigraphy has been developed in China for nearly 20 years. By the hard work of Chinese geologists, it went through three development stages which are beginning, high-speed development and mature development. Among the stages the Chinese geologists progressed quite a lot and acquired plentiful achievements especially in the research of regional sequence stratigraphy, theoretical sequence stratigraphy, sequence stratigraphy with mineral controlling, sequence stratigraphy in oil and gas exploration, high-resolution sequence stratigraphy, Milankovitch cycles, continental sequence stratigraphy (including alluvial system and desert aeolian system), applications of new techniques and methods in sequence stratigraphy (seism, well-log, computer simulation, neutron technique, cosmogenic nuclide etc.), dynamic sequence stratigraphy in basin depression and mountain building, sequence stratigraphy in the Tibet plateau and orogenic zones, diagenetic sequence stratigraphy, chemical sequence stratigraphy, tectonic sequence stratigraphy and sequence-lithofacies palaeogeography mapping etc. Based on the analysis of research status of Chinese sequence stratigraphy, it is suggested that Chinese geologist should enhance the application of sequence stratigraphy, and also should pay more attention to the basis research, technique improvement and feature development, in order to devote themselves to the development of sequence stratigraphy.
引文
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