Results 281 to 290 of about 22,659,233 (405)
Flexible joints for seismic-resilient design of masonry-infilled RC frames. [PDF]
Manojlovski F+30 more
europepmc +1 more source
Crater lakes in core regions of former ice sheets have the potential to preserve long‐term sedimentary archives that are otherwise rare in glaciated landscapes due to pervasive glacial erosion. Lake Wiyâshâkimî, an impact crater lake located in the inner core of the Québec‐Labrador Dome of the Laurentide Ice Sheet, provides a rare example of such a ...
Etienne Brouard, Patrick Lajeunesse
wiley +1 more source
Seismic characterization of lava flow facies in the critical zone of the deccan traps using shear wave velocity models. [PDF]
Sharma R+3 more
europepmc +1 more source
Low‐relief dry channels appear out of place across a glaciated karst landscape in northern Ohio. Channels are only a few metres deep cut into limestone and draped with a veneer of till. Several hypotheses are proposed for explaining the channels. Low‐relief dry channels are observed across the Bellevue‐Castalia Karst Plain of north‐central Ohio, USA ...
Timothy G. Fisher+6 more
wiley +1 more source
AVO reflectivity and pre-stack seismic impedance inversion for gas sand channel detection at South Abu El Naga Field, Onshore Nile Delta, Egypt. [PDF]
Al-Ashqar NA+3 more
europepmc +1 more source
SEISMIC HAZARD ANALYSIS USING A POLYGONAL SOURCE-AREA MODEL
Yutaka Ishikawa
openalex +2 more sources
This paper presents the results of a dual approach for assessing fossil benthic foraminiferal communities using both traditional morphology‐based analyses and sedimentary ancient DNA (sedaDNA) metabarcoding. The main objectives are to test the feasibility of sedaDNA analyses to assess foraminiferal biodiversity in temperate shelf sediments (Le Croisic,
Meryem Mojtahid+13 more
wiley +1 more source
Seismic performance of multistory frames with novel self-centering friction SMA dampers. [PDF]
Li W+5 more
europepmc +1 more source
High‐resolution LiDAR data with field validation of inferred southern Ontario ice stream terrains indicate that steady‐state ice streaming is difficult to reconcile with our observations. Rather, these new observations show strong evidence of significant fluvial scouring across the area in which meltwater sheet flow overtopped the landscape.
David R. Sharpe, Chris C. Smart
wiley +1 more source