Results 21 to 30 of about 1,337,965 (296)

Submarine volcano 8.10 (Kuril island arc)

open access: yesВестник Камчатской региональной ассоциации "Учебно-научный центр". Серия: Науки о Земле, 2022
The submarine volcano 8.10, part of the South Iturup group of underwater volcanoes of the Kuril island arc (KIA), was studied using a proven technology of quantitative interpretation of hydromagnetic survey materials in combination with echo sounding ...
Blokh Yu.I.   +7 more
doaj   +1 more source

The role of island-arc oceanic, collisional and intraplate magmatism in the formation of continental crust in the Mongolia-Trasnbaikalia region: geostructural, geochronological and Sm-Nd isotope data

open access: yesГеодинамика и тектонофизика, 2021
The formation of continental crust in the Mongolia-Transbaikalia region is researched to identify the mechanisms of interactions between the crust and the mantle in the development of the Neoarchean, Proterozoic and Paleozoic magmatic and sedimentary ...
I. V. Gordienko
doaj   +1 more source

SEISMOTECTONICS AND MECHANISMS OF TSUNAMI GENERATION ALONG ACTIVE BOUNDARIES OF YOUNG, MARGINAL SEA BASINS AND SPREADING RIDGES OF THE SOLOMON ISLANDS REGION – Case Study: The Earthquake and Tsunami of 1 April 2007 in the Solomon Islands [PDF]

open access: yesScience of Tsunami Hazards, 2020
The Solomon Islands region is characterized by high seismic activity. During the last 100 years there have been numerous strong earthquakes with periodic variation of recurrence.
George Pararas-Carayannis
doaj  

Reconstructing the Crustal Section of the Intra‐Oceanic Caribbean Island Arc: Constraints From the Cumulate Layered Gabbronorites and Pyroxenites of the Rio Boba Plutonic Sequence, Northern Dominican Republic

open access: yesGeochemistry, Geophysics, Geosystems, 2022
Located in northern Dominican Republic, the Early Cretaceous Rio Boba mafic‐ultramafic plutonic sequence constitutes a lower crust section of the Caribbean island arc, made up by gabbroic rocks and subordinate pyroxenite.
J. Escuder‐Viruete   +5 more
doaj   +1 more source

Expeditionary research on the Kronotsky Peninsula

open access: yesВестник Камчатской региональной ассоциации "Учебно-научный центр". Серия: Науки о Земле, 2023
The sublatitudinal active fault on the Kronotsky Peninsula (Kamchatka) has been studied. The deformations of the Holocene soil-pyroclastic cover opened by the trench indicate reverse vertical movements along the fault plane.
A.I. Kozhurin   +3 more
doaj   +1 more source

ARC 2006-21

open access: yes, 2009
Het Centraal Bodemkundig Bureau (CBB) uit Deventer heeft Archaeological Research & Consultancy (ARC bv) opdracht verleend voor het uitvoeren van een archeologisch inventariserend onderzoek (IVO) op een perceel naast Noldijk 84 in Barendrecht.
Wullink, A.J. (ARC b.v.)
core   +1 more source

Paleogeotectonic position of the Kyzyk Chadr copper-porphyry ore field (Republic of Tyva)

open access: yesРуды и металлы, 2023
Regional-scale localization conditions of the Kyzyk-Chadr molybdenum-copper porphyry ore field in the southern folded frame of the Siberian Platform are considered.
Starostin I. A.   +2 more
doaj   +1 more source

Contrasting Volcanic Deformation in Arc and Ocean Island Settings Due To Exsolution of Magmatic Water

open access: yesGeochemistry, Geophysics, Geosystems, 2022
Two of the most widely observed co‐eruptive volcanic phenomena—Ground deformation and volcanic outgassing—Are fundamentally linked via the mechanism of magma degassing and the development of compressibility, which controls how the volume of magma changes
Stanley Tze Hou Yip   +4 more
doaj   +1 more source

ARC-Publicaties 80

open access: yes, 2009
Bundel van klein regionaal onderzoek ...
ARC bv
core   +1 more source

Soft Skins With Reversible Thickness Morphing: Materials, Mechanisms, and Applications

open access: yesAdvanced Materials, EarlyView.
Evolution of electronic skin (e‐skin) technologies toward adaptive, multifunctional soft skins. Phase I highlights early rigid and discrete sensory interfaces. Phase II shows the transition toward flexible, stretchable, and large‐area e‐skin. Phase III captures the emergence of computational e‐skin.
Oliver Ozioko   +2 more
wiley   +1 more source

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