Temporal significance of sequence boundaries

Author:

Catuneanu Octavian,Willis Andrew J,Miall Andrew D

Publisher

Elsevier BV

Subject

Stratigraphy,Geology

Reference33 articles.

1. Relationship of eustatic oscillations to regressions and transgressions on passive continental margins. In: Price, R.A. (Ed.), Origin and Evolution of Sedimentary Basins and their Energy and Mineral Resources;Angevine;Am. Geophys. Union, Geophys. Monogr.,1989

2. Catuneanu, O., 1996. Reciprocal Architecture of Bearpaw and post-Bearpaw Sequences, Late Cretaceous–Early Tertiary, Western Canada Basin. Ph.D. thesis, University of Toronto, Toronto, 301 pp.

3. Reciprocal architecture of Bearpaw T–R sequences, uppermost Cretaceous, Western Canada Sedimentary Basin;Catuneanu;Bull. Can. Pet. Geol.,1997

4. Onlap, offlap, and the origin of unconformity-bounded depositional sequences;Christie-Blick;Mar. Geol.,1991

5. Stratigraphic record of Quaternary sea levels: implications for more ancient strata. In: Nummedal, D., Pilkey, O.H., Howard, J.D. (Eds.), Sea-Level Fluctuations and Coastal Evolution;Demarest;Soc. Econ. Paleontol. Mineral. Spec. Publ.,1987

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