Deciphering the sedimentological imprint of paleoseismic events: an example from the Aptian Codó Formation, northern Brazil
- 6 September 2000
- journal article
- Published by Elsevier in Sedimentary Geology
- Vol. 135 (1-4) , 137-156
- https://doi.org/10.1016/s0037-0738(00)00068-3
Abstract
No abstract availableKeywords
This publication has 40 references indexed in Scilit:
- Earthquake-induced structures in young sedimentsPublished by Elsevier ,2003
- Earthquake magnitude-frequency, epicentral distance, and soft-sediment deformation in sedimentary basinsPublished by Elsevier ,2003
- Facies architecture variations and seismogenic structures in the Carboniferous–Permian Saar–Nahe Basin (SW Germany): evidence for extension-related transfer fault activityPublished by Elsevier ,1998
- Molar-tooth structure in Proterozoic carbonate rocks: Origin from synsedimentary earthquakes, and implications for the nature and evolution of basins and marine sedimentGSA Bulletin, 1998
- Seismically induced soft-sediment deformation structures (seismites) around Sumdo in the lower Spiti valley (Tethys Himalaya)Sedimentary Geology, 1996
- Earthquakes and deformational structures (seismites) in Holocene sediments from the Himalayan-Andaman Arc, IndiaTectonophysics, 1987
- Genesis and diagnostic value of soft-sediment deformation structures—A reviewSedimentary Geology, 1983
- Convolute laminations — a theoretical analysis: example of a Pennsylvanian sandstoneSedimentary Geology, 1981
- Shear zones in granular materialRock Mechanics and Rock Engineering, 1977
- Dating of historical earthquakes by mud profiles of lake-bottom sedimentsNature, 1976