Results 81 to 90 of about 871 (186)
The North African section of the Gondwana margin was the site of voluminous, arc-related magmatism during the Late Neoproterozoic (Avalonian–Cadomian orogen).
P. ANDONAEGUI +2 more
doaj
ABSTRACT This research addresses the territorial organisation of metallurgical production during the El Argar Bronze Age (2200–1550 cal bc) in the inner areas of El Argar territory through lead‐isotope and trace element analyses of geological copper ores, archaeometallurgical remains and copper‐based artefacts.
M. Murillo‐Barroso +8 more
wiley +1 more source
ABSTRACT A quartz‐rich paragneiss from the Variscan Erzgebirge Crystalline Complex (ECC) was studied in detail because of abundant millimetre‐sized and clearly oriented pseudomorphs after a sodic mineral interpreted to have been jadeite. This mineral, or pseudomorphs after it, is rarely found in extensive high‐pressure (HP)–ultrahigh‐pressure (UHP ...
Hans‐Joachim Massonne
wiley +1 more source
Sun, Sea and Sand; Cretaceous Source to Sink Systems of Senegal, NW Africa
Source to sink exhumation models for the Senegalese Basin throughout the Cretaceous, combining Cretaceous vegetation, climate evolution, hinterland uplift, exhumation and paleo‐drainage evolution. Figure not to scale in order to emphasise the lateral unroofing of the Hercynian age Mauritanide Belt, eroding through the Gaouâ and Gadel group source rocks.
M. Pearson +3 more
wiley +1 more source
Exploitation of geothermal energy for the production of electric energy and warm for the town agglomeration of Litoměřice [PDF]
The Municipality of Litoměřice is very actively engaged in actions for an improvement of environmental conditions in the town as well as in its surroundings.The most appropriate solution seems to be the exploitation of geothermal energy using a HDR ...
Vlastimil Myslil, Václav Frydrych
doaj
The Cadomian basement of SW Iberian Massif appears in the so-called Ossa-Morena Complex, which contains several allochthonous terranes that are key for deciphering the evolution of the Gondwana margin during the Neoproterozoic.
Díez Fernández, Rubén +9 more
core +1 more source
In this work focussing on the Cenozoic continental carbonates of the Paris Basin, new information is brought to light on the spatialisation of continental carbonates facies thanks to correlations between coastal and palustrine environments. It presents arguments for distinguishing between marine (lagoon‐type) and continental (lake‐type) deposits based ...
Kévin Moreau +4 more
wiley +1 more source
New SHRIMP U-Pb zircon ages for the Portalegre and Alcáçovas orthogneisses document a complex pre- Variscan history for the Iberian basement in Portugal. The available geochemical and geochronological data for the Alcáçovas orthogneiss (ca.
Cordani Umberto G. +6 more
doaj
The late Precambrian Cadomian Orogen exposed in the North Armorican Massif (northwest France) is a collage of displaced terranes that, in part, developed during amalgamation of continental-arc and marginal-basin complexes.
R. S. D'Lemos +2 more
core +1 more source
Abstract Zircon U‐Pb‐He double dating (ZDD) provides the opportunity to derive high temperature crystallization ages and low temperature cooling ages from the very same mineral grain, making it especially attractive for zircon provenance studies. We present the combination of in situ detrital zircon U‐Pb‐He double dating and Raman spectroscopy‐based ...
I. Dunkl +4 more
wiley +1 more source

