Results 61 to 70 of about 5,545 (230)

Paleoseismology of the Xorxol Segment of the Central Altyn Tagh Fault, Xinjiang, China

open access: yesAnnals of Geophysics, 2003
Although the Altyn Tagh Fault (ATF) is thought to play a key role in accommodating India-Eurasian convergence, little is known about its earthquake history.
Z. Y. Qiao   +5 more
doaj   +1 more source

LiDAR and Paleoseismology Solve Earthquake Mystery in the Pacific Northwest, USA

open access: yesGeophysical Research Letters, 2021
One of the largest historical earthquakes in the U.S. Pacific Northwest occurred on December 15, 1872 near the south end of Lake Chelan. Lack of recognized surface deformation suggested that the earthquake occurred on a blind, perhaps deep, fault.
Brian L. Sherrod   +2 more
doaj   +1 more source

New Zealand Active Faults Database: the high‐resolution dataset v2.0

open access: yesNew Zealand Journal of Geology and Geophysics, Volume 68, Issue 5, Page 955-970, December 2025.
ABSTRACT The New Zealand Active Faults Database (NZAFD) contains underpinning data to help mitigate the impacts of future surface‐rupturing earthquakes in Aotearoa New Zealand. However, defining the associated hazards and risks must be undertaken at relevant scales and as such, the NZAFD contains two scale‐based datasets each serving complementary, but
Regine Morgenstern   +13 more
wiley   +1 more source

STUDI PALEOSEISMOLOGI AKIBAT BENCANA GEMPA BUMI DI ZONA SESAR KALIGARANG (KGFZ) DI SEMARANG

open access: yesTeknik, 2012
Earthquake in the past can study with paleoseismology. Kaligarang fault zone will record the event ofearthquake and result the sediment. The metode of research is detail field mapping and field excavation.Evidence of paleoseismology in the filed, we find
Fahrudin Fahrudin
doaj  

Along-strike extent of earthquakes on multi-segment reverse faults; insights from the Nevis-Cardrona Fault, Aotearoa New Zealand

open access: yesSeismica
Evaluating fault segmentation is important for our understanding of seismic hazard assessment and fault growth. However, it is still unclear what controls if reverse fault earthquakes will rupture across segment boundaries.
Jack Williams   +7 more
doaj   +1 more source

Lichenometry dating of coseismic changes to a New Zealand landslide complex

open access: yesAnnals of Geophysics, 2003
Lichenometry is a surface-exposure-dating procedure that complements traditional trench-and-date stratigraphic studies of earthquakes. Lichens on the surficial blocks of a slump in the Seaward Kaikoura Range, South Island, New Zealand provide ...
W. B. Bull
doaj   +1 more source

Insights into temporal earthquake clustering from the Settlement Fault, southeastern Otago, Aotearoa New Zealand

open access: yesNew Zealand Journal of Geology and Geophysics, Volume 68, Issue 4, Page 747-772, December 2025.
ABSTRACT We combine previous studies, fieldwork, lidar data, and trenching to examine late Quaternary activity of the SE‐dipping ≥23 km long Settlement Fault in the southeastern South Island. Trenching of a scarp crossing a small alluvial fan exposed a > 3 m thick sequence of folded sandy to silty fan alluvium.
Jack N. Williams   +4 more
wiley   +1 more source

Seismic Activity Along the Periadriatic and Sava Faults in the Past Two Millennia—An Archaeoseismological Assessment

open access: yesGeosciences
Most of the Periadriatic Fault System has been active during the Oligocene and Miocene times. Its western part seems to be almost inactive ever since, while the eastern segments show limited seismic activity.
Miklós Kázmér, Krzysztof Gaidzik
doaj   +1 more source

Paleoseismology of the North Anatolian Fault at Güzelköy (Ganos segment, Turkey): Size and recurrence time of earthquake ruptures west of the Sea of Marmara

open access: yes, 2012
International audienceThe Ganos fault is the westernmost segment of the North Anatolian Fault that experienced the Mw = 7.4 earthquake of 9 August 1912.
Aksoy, M. Ersen   +5 more
core   +5 more sources

Paleoseismic History of the Dead Sea Fault Zone [PDF]

open access: yes, 2015
International audienceThe aim of this entry is to describe the DSF as a transform plate boundary pointing out the rate of activedeformation, fault segmentation, and geometrical complexities as a control of earthquake ruptures.
A Agnon   +53 more
core   +2 more sources

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