Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Hasnaa Harmouzi"'
Autor:
Mohamed El Basri, Hasnaa Harmouzi, Lahcen El Basri, Mohamed Mastere, Ibrahim Ouchen, Bouchta El Fellah, Brahim Benzougagh
Publikováno v:
Iraqi Geological Journal, Vol 57, Iss 1B, Pp 55-66 (2024)
Indirect geophysical methods are increasingly associated with direct underground methods in investigating the subsurface to address environmental and geotechnical problems and reduce the cost of underground studies. These methods make it possible to
Externí odkaz:
https://doaj.org/article/d8957c16ecb946f7aa93bae23fd1b508
Publikováno v:
Geosciences, Vol 11, Iss 12, p 495 (2021)
This study presents the results of a landslide susceptibility analysis applied to the Vrancea-Buzău seismogenic region in the Carpathian Mountains, Romania. The target area is affected by a large diversity of landslide processes. Slopes are made-up
Externí odkaz:
https://doaj.org/article/8e13304b0ee5464e8260a086cb6a57d5
Morocco is one of the countries with a long geological history, tracing several orogenies. The most recent, called alpine, was at the origin of the formation of the Rifian chain by the collision of the two tectonic plates African and Eurasian. This a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8abfc9d05d8a5731a965a7c7fb1ab40b
https://doi.org/10.5194/egusphere-gc11-solidearth-2
https://doi.org/10.5194/egusphere-gc11-solidearth-2
Publikováno v:
Geosciences; Volume 11; Issue 12; Pages: 495
This study presents the results of a landslide susceptibility analysis applied to the Vrancea-Buzău seismogenic region in the Carpathian Mountains, Romania. The target area is affected by a large diversity of landslide processes. Slopes are made-up
Autor:
Candan Gokceoglu, Mohamed Rouai, Ebru Akcapinar Sezer, Hakan A. Nefeslioglu, Hasnaa Harmouzi, Abdelillah Dekayir
Publikováno v:
Arabian Journal of Geosciences. 12
The goal of this study was to experiment artificial neural network (ANN) classifier on various available physical factors in the study area to produce a reliable landslide susceptibility map. The mapping of landsides is classically established throug