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- W1569775383 abstract "Transgression during the upper Turonian in the area of the present-day Powder River basin was episodic: initial sea level rise, followed by a gradual overtaking of sea level rise by sedimentation rate, then another sea level rise to higher than it was before. Most of the parasequences produced consist of a transgressive lag directly overlain by coarsening-upward progradational deposits. Others are more complex. These more complex parasequences are composed of a transgressive lag overlain by fining-upward transgressive sediments overlain by coarsening-upward regressive deposits. A condensed section or omission surface separating the transgressive portion from the regressive portion is rarely found. Several such packages are found stacked vertically in areas that were near the basin margin. Farther paleolandward, part of the record preserved in the marine parasequences was removed by erosion. In the deeper parts of the basin, the condensed section encompasses part or all of the record. Capping the last progradational deposit in some locations in a shelf sand ridge. Understanding the details of sequence stratigraphy increases the accuracy of its use for predicting where to find reservoir sandstones. Certain Wall Creek facies, such as shelf sand ridges, are important petroleum reservoirs in the Powder River basin." @default.
- W1569775383 created "2016-06-24" @default.
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- W1569775383 date "1989-09-01" @default.
- W1569775383 modified "2023-09-23" @default.
- W1569775383 title "Transgressive parasequences in Cretaceous upper Frontier (Wall Creek) sandstone" @default.
- W1569775383 hasPublicationYear "1989" @default.
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