Physical and Thermal Properties Analysis of Hematite for Thermal Heat Storage. [PDF]
Santos A, Almeida F, Rocha F.
europepmc +1 more source
Cronología de los ciclos Cadomiense y Varisco en la Zona de Ossa Morena, SO de Iberia: magmatismo granítico desde la subducción a la extensión [PDF]
El estado de conocimiento sobre la Zona de Ossa Morena es variable. Existen estudios petrológicos, geoquímicos, isotópicos y geocronológicos sobre muchos cuerpos pero pocos son estudios de detalle de alguno de los mismos.
Salman, K.
core +1 more source
Contrasting magma types and timing of intrusion in the Permian layered mafic complex of Mont Collon (Western Alps, Valais, Switzerland): evidence from U/Pb zircon and 40Ar/39Ar amphibole dating [PDF]
.: We have selected and dated three contrasting rock-types representative of the magmatic activity within the Permian layered mafic complex of Mont Collon, Austroalpine Dent Blanche nappe, Western Alps.
Bussy, François +5 more
core
Foreword [al Special issue "The Ossa-Morena Zone (Iberian Massif): Geological findings at the turn of the 21st Century", de la revista "Journal of iberian geology", ISSN 1698-6180. [PDF]
Depto. de Mineralogía y PetrologíaFac.
Casquet, César
core
The Penacova-Régua-Verin (PRV) and the Manteigas-Vilariça-Bragança (MVB) are two of the longest faults of the Iberian Peninsula. These faults striking NNE–SSW, over lengths of >200 km, were developed during late-Variscan Orogeny and reactivated in ...
Sandra González-Muñoz +1 more
doaj +1 more source
The first petrographic characterisation of a prehistoric rock crystal mine in the Swiss Alps. [PDF]
Hess T, Mullis J, Franz L.
europepmc +1 more source
Mineral chemistry dataset of the Tournaisian - Lower Viséan submarine basaltic volcanism of the Matachel Basin (SW Iberian Massif). [PDF]
Sarrionandia F +5 more
europepmc +1 more source
Large plates and small blocks: The Variscan orogeny in the Bohemian Massif
The Bohemian Massif of the Central European Variscides consists of several late Proterozoic / early Paleozoic low-strain crustal units, namely the Bruno-Vistulian continental block of the Laurussian plate that is juxtaposed with the Tepla-Barrandian Unit and the Lausitz block of the Gondwana plate.
Kroner, U., Romer, R.
openaire +2 more sources
Alpine peak pressure and tectono-metamorphic history of the Monte Rosa nappe: evidence from the cirque du Véraz, upper Ayas valley, Italy. [PDF]
Vaughan-Hammon JD +3 more
europepmc +1 more source
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

