Participants learn how to recognize and correlate sequence boundaries, flooding surfaces, condensed sections, and system tracts.
学习人员学习如何识别和对比层序边界、水淹表面、致密剖面和体系区块。
Condensed sections are most commonly deposited during transgressions. In such cases they are associated with "maximum flooding surfaces" and form important sequence stratigraphic markers.
凝缩剖面最常见于海侵期的沉积，此种情况下，它们与“最大洪水面”相伴，并形成重要的层序地层学的标志层。
Identification of condensed section is not only the key to understanding of sequence structure, but also critical to analysis of global relative sea level changes during geologic history.
对凝缩段的识别不仅是认识层序结构的关键，而且对分析地质历史时期全球相对海平面变化至关重要。
The concept of condensed body, main controlling factors of lacustrine sedimentary sequence, classification of system tracts, and research methods of continental sequence stratigraphy are discussed.
在凝缩体的概念、陆相盆地中湖相沉积层序形成的主控因素、体系域的划分以及陆相层序地层学的研究方法等方面，提出了探讨性的意见。
The concept of condensed body, main controlling factors of lacustrine sedimentary sequence, classification of system tracts, and research methods of continental sequence stratigraphy are discussed.
在凝缩体的概念、陆相盆地中湖相沉积层序形成的主控因素、体系域的划分以及陆相层序地层学的研究方法等方面，提出了探讨性的意见。
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