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Insights into the seismogenesis and tectonic implications of an isolated intraplate earthquake (M4.0) on February 17, 2025, in Delhi [PDF]

open access: yesScientific Reports
On February 17, 2025, a magnitude 4.0 earthquake occurred near Jheel Park in South Delhi, approximately 6 km from the epicenter of the November 25, 2007, M4.6 event, one of the most significant regional earthquakes in recent decades.
Sanjay Kumar Prajapati   +4 more
doaj   +2 more sources

News, recent developments and progress

open access: yes地震科学进展, 2023
On the 50th anniversary of Progress in Earthquake Sciences, the scientific bibliometrics methods supplied by CiteSpace are used to conduct author collaboration network analysis and keyword co-occurrence analysis of the 7151 papers published in Recent ...
Wenyi Liu, Li Li, Wenqing Wang
doaj   +1 more source

Effect of Freeze-Thaw Cycles on Shear Strength Properties of Loess Reinforced with Lignin Fiber

open access: yesGeofluids, 2022
Freeze-thaw cycles caused by climate change can change the structure and strength of the soil. In seasonally frozen soil areas, the use of improved loess as a filling material must consider the effects of freeze-thaw cycles.
Zhongnan Gao   +5 more
doaj   +1 more source

The R package “eseis” – a software toolbox for environmental seismology [PDF]

open access: yesEarth Surface Dynamics, 2018
Environmental seismology is the study of the seismic signals emitted by Earth surface processes. This emerging research field is at the intersection of seismology, geomorphology, hydrology, meteorology, and further Earth science disciplines.
M. Dietze
doaj   +1 more source

SEISMICITY AND SEISMIC MONITORING OF MONTENEGRO

open access: yesAlbanian Journal of Natural and Technical Sciences, 2021
The coastal area encompassing the towns of Ulcinj, Bar, Budva and the entire Boka Bay is the most seismically active area in Montenegro. Going inland, the whole regions of Skadar Lake, Maganik mountain ridge, Polimlje river basin etc.
Nataša Kaluđerović   +1 more
doaj   +1 more source

Ometepec-Pinotepa Nacional, Mexico Earthquake of 20 March 2012 (Mw7.5): A preliminary report

open access: yesGeofísica Internacional, 2013
A partir de un análisis de los datos locales y regionales del sismo somero e inverso de Ometepec-Pinotepa Nacional (Mw 7.5), del 20 de marzo de 2012, se determinó la localización de su hipocentro en 16.254°N 98.531°W, aproximadamente 5 km fuera de la ...
UNAM Seismology Group
doaj   +1 more source

Papanoa, Mexico earthquake of 18 April 2014 ( M w 7.3)

open access: yesGeofísica Internacional, 2015
El sismo de Papanoa rompió la interfase de la placa al noroeste de la brecha sísmica de Guerrero. En esta región, los grandes sismos anteriores ocurrieron en 1943 (Ms 7.4), 1979 (Mw 7.4) y 1985 (Mw 7.5). El terremoto se registró en la región cercana a la
UNAM Seismology Group
doaj   +1 more source

Isotopes & Geochemistry: Tools For Geothermal Reservoir Characterization (Kamchatka Examples) [PDF]

open access: yesE3S Web of Conferences, 2019
The thermal, hydrogeological, and chemical processes affecting Kamchatka geothermal reservoirs were studied by using isotope and geochemistry data: (1) The Geysers Valley hydrothermal reservoirs; (2) The Paratunsky low temperature reservoirs; (3) The ...
Kiryukhin Alexey   +9 more
doaj   +1 more source

Review on Bougue gravity anomaly and crustal density structure in Sichuan-Yunnan and its adjacent areas

open access: yes地球与行星物理论评, 2022
Sichuan-Yunnan and its adjacent area are the main places where the eastward material flow from the Tibet Plateau escapes and spins to SE-SSE with active geological formations and frequent seismic activity.
Yutong Shen   +5 more
doaj   +1 more source

Identification of Modal Parameters for Reinforcement of Walls in Earthen Ruins

open access: yesAdvances in Materials Science and Engineering, 2021
The protection of earthen sites plays an important role in the context of preservation of cultural heritage, especially in the inheritance and promotion of history and culture.
Bei Liu   +4 more
doaj   +1 more source

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