Soft-sediment deformation in epicontinental carbonates as evidence of paleoseismicity with evidence for a possible new seismogenic indicator: Accordion folds

Author:

Ettensohn F.R.,Zhang C.,Gao L.,Lierman R.T.

Publisher

Elsevier BV

Subject

Stratigraphy,Geology

Reference58 articles.

1. Preface ― seismicity and sedimentation;Cita;Marine Geology,1984

2. Deformation of Scottish Quaternary sediment sequences by strong earthquake motion;Davenport,1987

3. Regressive facies in the upper Lexington Limestone: Tanglewood–Millersburg relationships;Ettensohn,1992

4. Evidence and implications of possible far-field responses to Taconian orogeny: Middle–Late Ordovician Lexington Platform and Sebree Trough, east-central United States;Ettensohn;Southeastern Geology,2002

5. Structural inversion and origin of a Late Ordovician (Trenton) carbonate buildup: evidence from the Tanglewood and Devils Hollow members, Lexington Limestone, central Kentucky (USA);Ettensohn;Palaeogeography, Palaeoclimatology, Palaeoecology,2004

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