Results 251 to 260 of about 757,045 (352)
An Entropic Explanation for Gutenberg‐Richter Scaling
Abstract We develop a simple explanation for Gutenberg‐Richter (G‐R) size scaling of earthquakes on a single fault. We discretize the fault and consider all possible contiguous ruptures at that level of discretization. In this static model, we assume that slip scales with rupture length, and that the rupture rates at each point along the fault are ...
M. T. Page, E. H. Field
wiley +1 more source
Detection and Mitigation of GNSS Gross Errors Utilizing the CEEMD and IQR Methods to Determine Sea Surface Height Using GNSS Buoys. [PDF]
Wang J, Yan S, Tu R, Zhang P.
europepmc +1 more source
Abstract Intraplate volcanism has long been linked to deep mantle plumes. However, recent studies showed that intraplate magmatism can originate from transition zone dynamics, where lower‐mantle plumes might be ponding, creating a Thermal Boundary Layer (TBL).
Yingying Li +5 more
wiley +1 more source
Two origins of the winter subsidence in and around the Arabian Peninsula. [PDF]
Usman M, Heki K.
europepmc +1 more source
Abstract Establishing a quantitative framework to evaluate the spatiotemporal patterns of slow earthquakes and to detect their anomalous activities is essential for understanding diverse slip behaviors on plate boundaries and seismic hazard assessment. In this study, we focus on deep tectonic tremors, which are one manifestation of slow earthquakes and
Seiya Yano, Satoshi Ide, Shunichi Nomura
wiley +1 more source
Augmented reality tools for mathematics and geoscience education. [PDF]
Kaźmierczak R +4 more
europepmc +1 more source
Abstract At the northern Hikurangi margin, Aotearoa New Zealand, slow slip events (SSEs) recur every 6–24 months to ∼ ${\sim} $30 km depth. Although shallow SSEs (0–10 km) are well‐studied offshore, the deeper portion (10–30 km) remains poorly understood, limiting insight into SSE initiation.
Amy Woodward +11 more
wiley +1 more source
Real time NL UPD estimation method based on a sliding time window. [PDF]
Wang S +5 more
europepmc +1 more source
Three Drivers of 21st‐Century Changes in Ocean Tides
Abstract Numerical model simulations are conducted to study the response of barotropic ocean tides to 21st‐century climate change, as manifested by sea level rise, increasing ocean stratification, and expanding Antarctic ice shelf cavities. Emphasis is placed on surface elevations, with projections of M2 ${\mathrm{M}}_{2}$, S2 ${\mathrm{S}}_{2}$, K1 ${\
Lana Opel +8 more
wiley +1 more source

