Results 11 to 20 of about 19,331 (230)

Assessment of Landslide Susceptibility of the Wiśnickie Foothills Mts. (The Flysch Carpathians, Poland) Using Selected Machine Learning Algorithms

open access: yesFrontiers in Earth Science, 2022
Landslides are well-known phenomena that cause significant changes to the relief of an area’s terrain, often causing damage to technical infrastructure and loss of life.
Tymoteusz Zydroń   +2 more
doaj   +1 more source

Taxonomy and biostratigraphy of new and emended species of Cenozoic deep-water agglutinated foraminifera from the Labrador and North Seas [PDF]

open access: yes, 1989
Deep marine, fine grained sedimentary strata of Maastrichtian through Miocene age in the Labrador and North Sea sedimentary basins are rich in agglutinated benthic foraminifera.
Gradstein, F. M., Kaminski, M. A.
core   +1 more source

Erosion processes in Slovene Istria – part 2: Badlands

open access: yesActa Geographica Slovenica, 2009
This article is a continuation of the article on soil erosion in submediterranean Slovene Istria from the first issue of the 2009 (49-1) journal. In this article we present geomorphic processes in the badlands of the same area (Dragonja River basin, SW ...
Matija Zorn
doaj   +1 more source

New Permo-Carboniferous geochemical data from central Thailand: implication for a volcanic arc model [PDF]

open access: yes, 1991
Current ideas and models of geotectonic reconstructions of Southeast Asia are reviewed and new data on Late Carboniferous through Middle Permian tuffites and sills from central Thailand are presented in the light of the problems of Southeast Asian ...
Altermann   +57 more
core   +1 more source

Some Remarks on the Use of Deterministic and Probabilistic Approaches in the Evaluation of Rock Slope Stability [PDF]

open access: yes, 2020
The rock slope stability assessment can be performed by means of deterministic and probabilistic approaches. As the deterministic analysis needs only representative values (generally, the mean value) for each physical and geo-mechanical parameter ...
BUDETTA, PAOLO
core   +1 more source

Role of Saravan Thrust Fault on Formation and Development of Saravan Catchment Basin [PDF]

open access: yesجغرافیا و توسعه, 2014
Development of drainage basins has close relation with geomorphologic and geologic parameters. Therefore, study the relation between structural parameters like faults and development of drainage basins has greatly considered in hydrology and hydrogeology
Ali Asqar Moridi Farimani   +1 more
doaj   +1 more source

Provenance of the Bosnian Flysch [PDF]

open access: yesSwiss Journal of Geosciences, 2008
Sandwiched between the Adriatic Carbonate Platform and the Dinaride Ophiolite Zone, the Bosnian Flysch forms a c. 3000 m thick, intensely folded stack of Upper Jurassic to Cretaceous mixed carbonate and siliciclastic sediments in the Dinarides. New petrographic, heavy mineral, zircon U/Pb and fission-track data as well as biostratigraphic evidence ...
Mikes, Tamas   +9 more
openaire   +5 more sources

Sedimentary processes and architecture of Upper Cretaceous deep-sea channel deposits : a case from the Skole Nappe, Polish Outer Carpathians [PDF]

open access: yes, 2018
Deep-sea channels are one of the architectonic elements, forming the main conduits for sand and gravel material in the turbidite depositional systems.
Łapcik, Piotr
core   +2 more sources

Biostratigraphical study of Lower Cretaceous Kašajina river beds and its importance for geology of NE Serbia [PDF]

open access: yesGeološki Anali Balkanskoga Poluostrva, 2002
This article presents results of detailed palynological study in the Lower Cretaceous Kašajina River Beds (Klokočevac, NE Serbia) and its importance for the geology of NE Serbia.
Ercegovac Marko   +2 more
doaj   +1 more source

Analysis of the Flysch [PDF]

open access: yesNature, 1966
Sedimentary Features of Flysch and Greywackes By S. Dzulynski and E. K. Walton. (Developments in Sedimentology, Vol. 7.) Pp. viii + 274. (Amsterdam, London and New York: Elsevier Publishing Company, 1965.) 95s.
openaire   +1 more source

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