沉积沉积环境
地层学
地质学
年代地层学
口译(哲学)
体积热力学
领域(数学分析)
地球物理成像
地貌学
地震学
古生物学
计算机科学
沉积岩
构造学
数学分析
物理
数学
构造盆地
量子力学
程序设计语言
出处
期刊:The leading edge
[Society of Exploration Geophysicists]
日期:2013-02-01
卷期号:32 (2): 146-153
被引量:7
标识
DOI:10.1190/tle32020146.1
摘要
The presence of complex structure on seismic data often makes it difficult to recognize and interpret depositional systems in the volume. A number of techniques, under the broad topic of chronostratigraphy, have been developed in recent years to address this problem and enable more complete imaging and interpretation of seismic geomorphology and stratigraphy. A “domain transform” (DT) is an interpretation-guided process designed to remove some or all structural deformation from a seismic volume. It improves the imaging of paleo-depositional systems by creating a volume that consists of approximations of paleo-depositional surfaces. Such volumes are ideal for imaging, analysis, and interpretation of seismic geomorphology and stratigraphy.
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