Results 181 to 190 of about 9,466 (220)
Some of the next articles are maybe not open access.

Tectonic evolution of an intraplate basin: the Lower Tagus Cenozoic Basin, Portugal

Basin Research, 2016
AbstractThis article focuses on the reinterpretation of well, seismic reflection, magnetic, gravimetric, surface wave and geological surface data, together with the acquisition of seismic noise data to study the Lower Tagus Cenozoic Basin tectono‐sedimentary evolution.
João Carvalho   +7 more
openaire   +1 more source

Widespread ca. 1.4 Ga intraplate magmatism and tectonics in a growing Amazonia

GFF, 2015
AbstractHigh-quality U–Pb (Isotope Dilution-Thermal Ionisation Mass Spectrometry; ID-TIMS) baddeleyite ages were obtained for the Salto do Ceu (SC) gabbroic sill (1439 ± 4 Ma) and Nova Lacerda mafic dyke swarm (1387 ± 17 Ma) located ca. 150 km apart in the Jauru terrane (Paleo- to Mesoproterozoic) – SW Amazonia.
Wilson Teixeira   +5 more
openaire   +1 more source

Tectonics and magmatism of intraplate oceanic rises and the hot-spot hypothesis

Geotectonics, 2008
The brief characteristics of the large intraplate rises of the Indian and Atlantic oceans—the Ninetyeast, Mascarene, Maldives, and Walvis ridges and the Kerguelen Plateau—are discussed. The formation of these, as well as many other intraplate ridges, plateaus, and islands, is usually thought to be a result of the function of long-lived stationary deep ...
A. V. Artamonov, B. P. Zolotarev
openaire   +1 more source

Apparent stress and stress drop for intraplate earthquakes and tectonic stress in the plates

pure and applied geophysics, 1977
The magnitude of shear stress in the lithosphere is bounded from below by the apparent stress and stress drop during intraplate earthquakes. Apparent stresses and stress drops for a number of mid-plate earthquakes are calculated from the earthquake magnitude, SH wave amplitude spectra, and estimates of the length of the fault zone.
Randall M. Richardson, Sean C. Solomon
openaire   +1 more source

Hotspots and mantle plumes: global intraplate tectonics, magmatism and ore deposits

Mineralogy and Petrology, 2004
Intraplate tectono-magmatic phenomena, including the emplacement of layered intrusions, and the giant dyke swarms, anorogenic (hotspot) volcanism, oceanic plataeux, rifting processes, basin formation, and geomorphological features are discussed in the context of the mantle plume theory.
openaire   +1 more source

The structure and tectonics of the intraplate deformation area in the Indian Ocean

Tectonophysics, 1988
Abstract Intense tectonic deformations of sediments and basement unusual for the interior of the oceanic lithosphere plates can be seen on seismic reflection profiles from the northern Central Indian Basin. 10,000-mile long CSP profiles collected by the P.P.
Yuri P. Neprochnov   +3 more
openaire   +1 more source

Classification of intracontinental (intraplate) orogeny based on tectonics and its evolution

Since last 1960’s, the plate tectonics has been played a main role for the study on the Earth’s evolution and global tectonics, but mostly focused on the global divergence and convergence, and focused on the continental margin—subduction and collision.
Yu Wang, Songnan Liu, Mo Gong
openaire   +1 more source

Variscan tectonics of central Europe: Postaccretionary intraplate deformation of weak continental lithosphere

Tectonics, 1996
The area occupied by the Variscan belt of central Europe forms part of Gondwana‐derived microplates (essentially Avalonia and Armorica) that, according to paleomagnetic data, juxtaposed Baltica and Laurentia from the Upper Ordovician to the Lower Devonian.
openaire   +1 more source

INTRAPLATE VS INTERPLATE TECTONICS: DELINEATING TECTONIC ACTIVITY BY UTILIZING A TECTONIC-BASED GIS

Geological Society of America Abstracts with Programs, 2003
Jacob Yates III   +2 more
openaire   +1 more source

Intraplate magmatism and tectonics of southern Africa

Journal of African Earth Sciences, 1999
Paul Dirks   +2 more
openaire   +1 more source

Home - About - Disclaimer - Privacy