Results 51 to 60 of about 250 (169)
Abstract The Alpine Fault (AF) in Aotearoa New Zealand is a fast‐slipping plate boundary fault late in its seismic cycle that presents a major source of seismic hazard. Past earthquakes have created a structural‐geomorphic record of surface ruptures that we map and analyze for the northern AF using 1,000 km2 ${\text{km}}^{2}$ of Light Detection and ...
J. La Greca +5 more
wiley +1 more source
Do Large Earthquakes Occur at Regular Intervals Through Time? A Perspective From the Geologic Record
We analyzed a catalog of 31 published earthquake chronologies to assess the commonality of quasiperiodic earthquake recurrence across a range of fault types and tectonic settings.
Randolph T. Williams +2 more
doaj +1 more source
Impact of Anaerobic Cold Storage on Subseafloor Microbial Communities
Abstract Sediment cores recovered from the deep sea often cannot be sampled for microbiological analysis immediately due to the need for core splitting and processing for subsequent onboard measurements and core storage. Consequently, sections are often stored at 4°C under anaerobic conditions for extended periods.
Tastuhiko Hoshino +6 more
wiley +1 more source
Surface ruptures appear over a wide area in addition to the primary fault during a Large earthquake like the 2016 Kumamoto earthquake. Although the displacement of such distributed surface ruptures is small, information on their paleo activities provides
Daisuke Ishimura +5 more
doaj +1 more source
Implications of some early Jewish sources for estimates of earthquake hazardin the Holy Land
For the past two millennia the Holy Land was under the yoke of successive invaders and oppressors, not a fertile ground for growth of historiographic traditions.
I. Karcz
doaj +1 more source
New Zealand Active Faults Database: the high‐resolution dataset v2.0
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
The Manyas fault zone (southern Marmara region, NW Turkey): active tectonics and paleoseismology
The Manyas fault zone (MFZ) is a splay fault of the Yenice Gönen Fault, which is located on the southern branch of the North Anatolian Fault System. The MFZ is a 38 km long, WNW–ESE-trending and normal fault zone comprised of three en-echelon segments ...
Akın Kürçer +5 more
doaj +1 more source
During paleoseismological investigations on the seismogenic structure responsible for the 1915 earthquake in the Fucino Plain (Central Italy), some trenches were excavated at the intersection between Roman-age channels and a fault characterized by ...
P. Galli, F. Galadini
doaj +1 more source
Application of Tree-Ring Analysis to Paleoseismology [PDF]
Knowledge of a region's seismicity is one of the keys to estimating earthquake hazards. Unfortunately, historical records are generally inadequate for evaluations of seismicity. Paleoseismology addresses this problem using various techniques for dating earthquake‐disturbed materials.
openaire +1 more source
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

