Results 31 to 40 of about 208,858 (207)

Geological and geotechnical characterization of Ziragn Dam sitting, northwestern Ethiopia

open access: yesEnvironmental and Sustainability Indicators, 2023
The goal of this study was to look at the geological and geotechnical conditions of the Ziragn dam, which would be built across the Ziragn river for irrigation purposes.
Degu Birhanu, Chalachew Tesfa
doaj   +1 more source

Effect of sedimentary heterogeneities in the sealing formation on predictive analysis of geological CO2 storage [PDF]

open access: yes, 2019
Numerical models of geologic carbon sequestration (GCS) in saline aquifers use multiphase fluid flow-characteristic curves (relative permeability and capillary pressure) to represent the interactions of the non-wetting CO2 and the wetting brine. Relative
Alkan   +69 more
core   +2 more sources

Ages of the Pliocene-Pleistocene Alexandra and Ngatutura Volcanics, western North Island, New Zealand, and some geological implications [PDF]

open access: yes, 1989
The Alexandra and Ngatutura Volcanics are the two southernmost of the Pliocene-Quaternary volcanic fields of western and northern North Island, New Zealand, northwest of Taupo Volcanic Zone TVZ.
Briggs, Roger M.   +3 more
core   +2 more sources

Rare earth elements in clay-sized fractions: Implications for weathering fingerprint from parent materials to soils

open access: yesGeoderma
Rare earth elements (REEs) have gained attention as tracers of pedogenic processes over the last few decades. Clay-sized fractions (CSFs, < 2 μm) may play a crucial role in hosting REEs. To better understand the pedochemical signals of REEs in clay-sized
Xianming Zhang   +8 more
doaj   +1 more source

ORIGIN AND DISTRIBUTION OF CLAY MINERALS IN THE MUDSTONES OF THE KOLOSH FORMATION INRAWANDOZ AREA, NORTHEASTERN IRAQ

open access: yesIraqi Geological Journal, 2018
The mudstone/ shale units constituted 60% of the Kolosh Formation of 170 m thickness, which were studied and the clay minerals were identified to conclude the origin and paleoclimate.
Iqbal j. Mohammed   +1 more
doaj   +1 more source

Selenium in certain metamorphic rocks [PDF]

open access: yesBulletin of the Geological Society of Finland, 1973
The selenium contents of Precambrian metamorphic rocks from Finland were studied and tentative averages are presented. The pattern of the distribution of selenium in metamorphic rocks can be summarized as follows: Selenium most probably does not enter ...
T. Koljonen
doaj   +1 more source

Improving rock classification in terms of explosivity [PDF]

open access: yes, 2019
Purpose. To improve rock classification in terms of explosivity relying upon the detailed analysis of characteristics of rating classifications available in the Russian Federation and in the world. Methods.
Kirsanov, A   +5 more
core   +1 more source

Індивідуальне моделювання електропровідності поліміктових глинистих газонасичених пісковиків [PDF]

open access: yes, 2012
Гірські породи, які представляють продуктивні горизонти багатьох нафтогазових родовищ України, характеризуються неоднорідністю мінерального складу скелета породи, а також вторинними процесами породоутворення і відносяться до складнопобудованих порід ...
Коваль, Я. М.   +2 more
core  

Investigation on thermal property parameters characteristics of rocks and its influence factors

open access: yesNatural Gas Industry B, 2020
In this paper, the thermal property parameters of rocks from different lithology were studied with the cores from the different formation in Sichuan Basin and Tarim Basin as the research objects.
Jian Xiong   +5 more
doaj   +1 more source

Dielectric Dispersion Responses for Clay-Bearing Rocks Based on Digital Cores and Numerical Simulation

open access: yesApplied Sciences
The dielectric response of clay-bearing rocks is complex, which seriously affects the evaluation of oil saturation. This paper introduces the dual-Debye model to characterize the dielectric dispersion characteristics of pore water and the Debye model to ...
Jianshen Gao, Jiang Wang, Kun Liu
doaj   +1 more source

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