Symmetrical and upward shallowing cycles in the Middle Devonian of New York State and their implications for the punctuated Aggradational Cycle Hypothesis

Author:

Brett Carlton E.,Baird Gordon C.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Reference49 articles.

1. Calcareous Tempestites: Storm-dominated Stratification in Upper Muschelkalk Limestones (Middle Trias, SW-Germany)

2. Storm depositional dynamics: Dynamic stratigraphy in modern and ancient shallow marine sequences;Aigner,1985

3. Episodic accumulation and the origin of formation boundaries in the Helderberg Group of New York State;Anderson;Geology,1984

4. Pebbly phosphorites in shale: A key to recognition of a widespread submarine discontinuity in the Middle Devonian of New York;Baird;J. Sediment. Petrol.,1978

5. Sedimentary relationships of Portland Point and associated Middle Devonian rocks in central and western New York;Baird;N. Y. State Mus. Sci. Serv. Bull.,1979

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