Discontinuity surfaces and microfacies in a storm-dominated shallow Epeiric Sea, Devonian Cedar Valley Group, Iowa-Reference-Cited by-同舟云学术

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Discontinuity surfaces and microfacies in a storm-dominated shallow Epeiric Sea, Devonian Cedar Valley Group, Iowa

Published:2017-07-14 Issue:2 Volume:3 Page:136-160
ISSN:2055-4877
Container-title:The Depositional Record
language:en
Short-container-title:Depositional Rec

Author:

Brady Mara¹^ORCID,Bowie Christopher¹

Affiliation:

1. Department of Earth and Environmental Sciences; California State University, Fresno; 2576 East San Ramon Avenue, M/S ST-24 Fresno CA 93740 USA

Funder

American Association of Petroleum Geologists

California State University, Fresno

Publisher

Wiley

Subject

Paleontology,Stratigraphy,Geology,Environmental Science (miscellaneous),Oceanography

Reference80 articles.

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

2. Circulation in large ancient epicontinental seas: what was different and why?;Allison;Palaios,2006

3. Switching off the carbonate factory: a-tidality, stratification and brackish wedges in epeiric seas;Allison;Sed. Geol.,2005

4. Proximal-distal facies relationships and sedimentary processes in a storm dominated carbonate ramp (Kimmeridgian, northwest of the Iberian Ranges, Spain);Bádenas;Sed. Geol.,2001

5. Genesis of unusual lithologies associated with the Late Middle Devonian Taghanic biocrisis in the type Taghanic succession of New York State and Pennsylvania;Baird;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2012

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