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Titlebook: Cretaceous Resources, Events and Rhythms; Background and Plans R. N. Ginsburg,Bernard Beaudoin Book 1990 Springer Science+Business Media Do

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Relevance of Cretaceous Volcanic Activity to CRERIntense, global volcanic activity with peaks in the Aptian-Albian and Campanian-Maestrichtian may have had significant effects on sea level changes, paleobathymetry and circulation of the Pacific Ocean, chemistry of the atmosphere and hydrosphere and global climates, and the distribution and evolution of faunas and floras.
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Cretaceous Stage Boundaries — ProposalsA unified scale of Cretaceous stages has been generally accepted for a long time. However, the earliest stage, the Berriasian, is often replaced by the Ryazanian, reflecting the particular difficulties of correlating between the Tethyan and the Boreal Realms around the Jurassic-Cretaceous boundary.
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https://doi.org/10.1007/978-94-015-6861-6Cretaceous; research; economic geology
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,Räume als Wettbewerbseinheiten,le of eustasy in the formation of unconformity-bounded depositional sequences. The advantage of the sequence-stratigraphic approach is that unlike transgressions and regressions of the shoreline or changes in paleobathymetry, the development of prominent sequence boundaries is relatively insensitive
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,Räume als Wettbewerbseinheiten,unctuated by unconformities. The magnitude of erosion, thicknesses and facies distribution are influenced by subtle penecontemporaneous tectonics characteristic of the cratonic portion of the large Western Interior foreland basin..These Albian-age strata contain 3 sequences related primarily to sea
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y is deduced from (a) the degree of aggradation versus progradation of coastal sandbodies, (b) paleoenvironmental interpretation of the successive depositional systems tracts, (c) location and extent of basin-margin subaerial unconformities, (d) location and extent of marine condensed sections and t
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equence stratigraphy concepts and the synchronism between local depositional sequences and global eustatic cycles. Three sequence boundaries and three events identified as condensed sections have been correlated with the global cycle chart of Haq (1987) but within the sequences there are several pro
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