Results 131 to 140 of about 250 (169)
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Chapter 4 Paleoseismology of Volcanic Environments

1996
Publisher Summary This chapter discusses the paleoseismology of volcanic environments. It presents a criterion for the recognition of magma-induced, extensional structures to alleviate their misinterpretation in the paleoseismic record as products of single, large magnitude earthquakes.
William R. Hackett   +2 more
openaire   +1 more source

Submarine Paleoseismology Based on Turbidite Records

Annual Review of Marine Science, 2011
Many of the largest earthquakes are generated at subduction zones or other plate boundary fault systems near enough to the coast that marine environments may record evidence of them. During and shortly after large earthquakes in the coastal and marine environments, a spectrum of evidence may be left behind, mirroring onshore paleoseismic evidence ...
openaire   +2 more sources

Paleoseismology: evidence of earth activity

International Journal of Earth Sciences, 2016
The paleoseismic research aims to document earth activity during earthquakes, such as displacements of fault, rupture location, distribution of slip or ground shaking intensity. The earthquakes are usually distributed on the plate boundaries causing big damages of life on the Earth.
openaire   +1 more source

Paleoseismological Studies

2022
Hisao Kondo   +2 more
openaire   +1 more source

Paleoseismology of the Hyde Fault, Otago, New Zealand

New Zealand Journal of Geology, and Geophysics, 2022
David Barrell   +2 more
exaly  

Neotectonics and paleoseismology of the North Tabriz Fault, Azerbaijan Region, Northwest Iran

Journal of Asian Earth Sciences, 2023
Negar Haghipour   +2 more
exaly  

Paleoseismology of the Akatore Fault, Otago, New Zealand

New Zealand Journal of Geology, and Geophysics, 2020
Nicola Litchfield   +2 more
exaly  

5.12 Paleoseismology

2013
H. Kondo, L.A. Owen
openaire   +1 more source

History, status and trend about the research of paleoseismology

Science Bulletin, 1999
Yongkang Ran, Ran Yongkang
exaly  

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