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Use of Fischer plots to define third-order sea-level curves in Ordovician peritidal cyclic carbonates, Appalachians

J. F. Read and R. K. Goldhammer
Use of Fischer plots to define third-order sea-level curves in Ordovician peritidal cyclic carbonates, Appalachians
Geology (Boulder) (October 1988) 16 (10): 895-899

Abstract

Fischer plots in which cumulative cycle thickness corrected for linear subsidence is plotted against time were originally used in the study of Triassic peritidal sequences to define short-duration departures in relative sea level in the Milankovitch range (10 (super 4) to 10 (super 5) yr). However, they also provide a means of assessing magnitude of third-order (1 to 10 m.y.) fluctuations in sea level which, on the basis of their regional correlatability, we ascribe to eustatic events.


ISSN: 0091-7613
EISSN: 1943-2682
Coden: GLGYBA
Serial Title: Geology (Boulder)
Serial Volume: 16
Serial Issue: 10
Title: Use of Fischer plots to define third-order sea-level curves in Ordovician peritidal cyclic carbonates, Appalachians
Affiliation: Va. Polytech. Inst. and State Univ., Dep. Geol. Sci., Blacksburg, VA, United States
Pages: 895-899
Published: 198810
Text Language: English
Publisher: Geological Society of America (GSA), Boulder, CO, United States
References: 20
Accession Number: 1988-071110
Categories: Sedimentary petrologyStratigraphy
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus.
N33°00'00" - N47°30'00", W87°00'00" - W67°00'00"
Secondary Affiliation: Johns Hopkins Univ., USA, United States
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2017, American Geosciences Institute.
Update Code: 1988

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