Results 41 to 50 of about 5,012 (243)
The evolution of the foredeeps which developed on the northern Adriatic foreland took piace in a regime of oblique convergence. From the Late Oligocene onwards much compression in the Southern Alps must have been the compressional component of dextral ...
FRANCESCO MASSARI
doaj +1 more source
Ferroan granites (585-530 Ma) in the Transversal subprovince of the Borborema Province (BP) comprise two groups: G1) slightly peraluminous to metaluminous, alkali-calcic rocks (Aroeiras Complex and Serra Branca - Coxixola dike swarms (SBCDS)); G2 ...
José Victor Antunes de Amorim +5 more
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Shape and intrusion history of the Late Caledonian Newry Igneous Complex, Northern Ireland [PDF]
The Tellus high-resolution airborne magnetic and radiometric maps define previously unmapped zones within the Newry Igneous Complex, County Down. High-precision uranium–lead zircon dating of nine rock samples from different parts of the complex provides ...
Anderson, Paul +6 more
core +1 more source
Negative structures of the Earth’s crust, including intermountain and intramountain basins, are key sources of information on the formation of the continental crust through plate tectonic and orogenic cycles.
M. G. Leonov +5 more
doaj +1 more source
The basement’s top tectonics of the East European platform (EEP) has been considered on the basis of the modern mapping data. The importance of the long-lived tectonic zones that form the vortex megastructure has been justified.Their Riphean — early ...
S. Y. Kolodyazhny
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Adakite-like geochemical signature (high Sr/Y ratio at a low Y concentration) is recognized in andesites and dacites, associated with intraplate basalts in the Orlov volcanic field of Sakhalin Island.
Sergei V. Rasskazov +5 more
doaj +1 more source
The Late Cretaceous is an important geological time interval for the Tibetan Plateau because it corresponds to the period when the tectonic regime changed from Lhasa‐Qiangtang collision to Indo‐Asian assembly.
Xin-Song Wang +5 more
semanticscholar +1 more source
Abstract Ribbon collision is a process that can rapidly disturb the symmetry of subduction zones. Previous studies have demonstrated how ribbon collision causes rotation at the surface and contortion in the slab, but have only focused on the surface kinematics.
Andres Rodriguez‐Corcho +4 more
wiley +1 more source
Critical Tectonic Limits for Geothermal Aquifer Use: Case Study from the East Slovakian Basin Rim
The Pannonian basin is a major geothermal heat system in Central Europe. Its peripheral basin, the East Slovakian basin, is an example of a geothermal structure with a linear, directed heat flow ranging from 90 to 100 mW/m2 from west to east.
Stanislav Jacko +4 more
doaj +1 more source
Abstract The Appalachian‐Caledonian orogen was built during the Paleozoic by accretion of peri‐Gondwanan terranes onto Laurentia, culminating in the formation of Pangea. During the Mesozoic, Pangea broke apart, displacing one section of the belt to eastern North America and another to northwestern Europe.
Roberto Masis +4 more
wiley +1 more source

