--> A Method to Interpret Cycle Stratigraphic Framework at Wireline Log-Resolution Using Seismic Data
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A Method to Interpret Cycle Stratigraphic Framework at Wireline Log-Resolution Using Previous HitSeismicNext Hit Data

Abstract

To interpret high-resolution (or log-level, meters to low tens of meter scale) sequence stratigraphic framework by using wireline-log data is a standard procedure pioneered by Van Wagoner et al. (1990). A high-resolution sequence framework directly from 3D Previous HitseismicNext Hit data, however, is a formidable task, if not just a dream. Previous HitSeismicNext Hit visual resolution is primarily dependent on the predominant frequency (15-60 Hz, depending on data quality and depth), not the bandwidth of the data, which is typically about half of the high-frequency limit and is too low for high-resolution interpretation. Also, a Previous HitseismicNext Hit reflection is basically referred to a reflection surface, not thickness of a stratal unit. Continuity of a reflection does not necessarily represent stratal continuity because of the amplitude tuning effect. As a result, high-resolution sequence stratigraphy has been reserved for outcrop and core/wireline log studies. Direct Previous HitseismicNext Hit correlation of higher-order sequences is more symbolic than real. Some progress has been made by a three-step process. First, Previous HitseismicNext Hit cube was converted to relative impedance volume, such that a Previous HitseismicNext Hit event can be viewed as representing a stratal unit. Then, the converted Previous HitseismicNext Hit volume was properly decomposed into selected panels of high, moderate, and low frequency components. Finally, a combined rendering of these panels was realized by using RGB or other color-blending schemes, creating a new display of Previous HitseismicNext Hit sections. A Previous HitseismicNext Hit Previous HitmodelingNext Hit study based on a geologically realistic sandstone-shale model revealed value to use the method to achieve a good tie between impedance (lithology or gamma ray) trace and its Previous HitseismicNext Hit response and to drastically improve Previous HitseismicNext Hit visual resolution and true stratal continuity. In the new display, the designated colors and the width of a Previous HitseismicNext Hit event both indicate thickness of a lithofacies unit. Sand content (or clay content) cycles, therefore, can be identified in a way similar to interpretation of gamma ray logs, with adequate resolution to correlation high-resolution sequences. To verify the results, controlled tests were done on previously published case studies with dense well control in GOM and lacustrine basins in China. In all those examples, high-resolution cycle stratigraphy was able to be established quickly using 3D Previous HitseismicTop data, with a resolution similar to gamma ray-based sequence-stratigraphic framework and comparable interpretation of SB, mfs, and systems tracts.