摘要
沉积学的概念源于１９世纪初，其发展大致经历了沉积岩石学、沉积学、沉积地质学三个阶段。目前，随着各种边缘、分支、交叉及横断学科的发展，沉积学研究取得了重大进展，主要表现在层序地层学、事件沉积学、矿床沉积学、实验沉积学、大地构造沉积学、储层沉积学、全球旋回地层学等的诞生和发展。预计到２１世纪，沉积学除在大陆动力学、全球变化方面进一步深入发展外，还将与资源和环境密切结合，形成新的学科领域，主要包括资源沉积学、环境沉积学、大陆动力沉积学、全球变化沉积学诸方面，进而为人类生存与发展作出重大的贡献。
The concept of sedimentology originated from the 19th century and underwent 3 development stages: sedimentary petrology, sedimentology, and sedimentary geology. Untill now, with the development of series of frontier , branch , intersect , and cross discinplines, sedimentology develops rapidly, including sequence stratigraphy , event sedimentology, deposit sedimentology, experimental sedimentology, tectonic sedimentoloy, reservoir sedimentology, global cyclestratigraphy etc.. By the time of the 21th century, sedimentology will not only develop further in aspects of geodynamies and global change etc., but form new fields of discinplines by combining with resource and environmental sciences. They are: (1)resource sedimentology, (2)environmental sedimentology, (3)geodynamic sedimentology, and (4) global change sedimentology etc..
出处
《成都理工学院学报》
CSCD
1999年第1期1-7,共7页
Journal of Chengdu University of Technology
关键词
沉积学
层序地层学
大陆动力沉积学
环境沉积学
sedimentology
sequence stratigraphy
geodynamic sedimentology
global change sedimentology
environmental sedimentology
resource sedimentology
