Results 11 to 20 of about 5,012 (243)
The El Salvador Fault Zone (ESFZ) is part of the Central American Volcanic Arc and accommodates the oblique separation movement between the forearc sliver and the Chortis block (Caribbean Plate).
Jorge Alonso-Henar +8 more
doaj +2 more sources
Bathymetric and seismic data provide insights into the geomorphological configuration, seismic stratigraphy, structure, and evolution of the area between Santorini, Amorgos, Astypalea, and Anafi islands.
Konstantina Tsampouraki-Kraounaki +8 more
doaj +2 more sources
Offshore data in the western Ionian Sea indicate that the NW–SE-trending dextral shear zone of the Alfeo-Etna Fault System turns to the N–S direction near the Ionian coastline, where the extensional Timpe Fault System is located.
Salvatore Gambino +8 more
doaj +2 more sources
The area of southeastern Papua New Guinea includes three active microplates – the Trobriand, Woodlark, and Solomon Sea plates – that are being deformed by regional convergence between the much larger Pacific and Australian Plates.
Lei Sun, Paul Mann
doaj +2 more sources
Multi-sensor satellite imagery data promote fast, cost-efficient regional geological mapping that constantly forms a criterion for successful gold exploration programs in harsh and inaccessible regions.
Basem Zoheir +3 more
doaj +2 more sources
Carbonatitic dykes during Pangaea transtension (Pelagonian Zone, Greece)
ISSN:0024 ...
Schenker, Filippo L. +4 more
openaire +4 more sources
Introduction. Transtension is a system of stresses that tends to cause oblique extension, i.e. combined extension and strike slip. Syn-volcanic transtensional deformations of the lithosphere may provide two possible scenarios for control of magmatic ...
S. V. Rasskazov +7 more
doaj +2 more sources
The role of transtension and transpression in incipient collision: insights from offshore SE Taiwan
Offshore SE Taiwan is regarded as the northern extension of the North Luzon Trough and reflects the early stages of arc–continent collision resulting from the oblique convergence between the Eurasian continental margin and the Luzon Arc.
Chian-Yu Huang +7 more
doaj +2 more sources
Abstract Dykes and minor eruptive vents are not randomly distributed within tectonically controlled volcanic arcs, which is reflected in the resulting morphology of stratovolcanoes. As a first-order approach, regional stress field controls the spatial distribution and geometry of dykes and minor eruptive vents.
Sielfeld, Gerd +2 more
openaire +5 more sources
General transpression and transtension
Carlos Fernández +2 more
openaire +2 more sources

