457 resultados para Marrón Emperador
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Mode of access: Internet.
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Mode of access: Internet.
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Mode of access: Internet.
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Incluye con portadilla propia en el tomo 2º: Animadversiones in Constantini Porphyrogeniti libros De themathibus et De administrando imperio.
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Incluye: Glossarium Annaeum, sive Declaratio verborum quae singulari aut rara notione usurpantur ab Anna Comnena ; Davidis Hoeschelii Augustani in Annae Comnenae Alexiadem praefationes ac notae, ex editione anni MDCX ; Caroli du Fresne Ambiani, Dom. du Cange, regi a consiliis, et Franciae quaestoris, in historiam Comnenicam, notae historicae et philologicae, praemittuntur ad pleniorem ejusdem historiae notitiam descriptio Constantinopoleos, ex Christophoro de Bondelmontibus, & indices genealogici Ducarum, Bryenniorum, Comnenorum, Ducum Apuliae, & Sultanorum Turcicorum & Iconiensium.
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Incluye con portadilla propia: Petri Possini e Societate Jesu Observationum Pachymerianarum ad historiam rerum Michaelis Palaeologi libri tres ; Appendix ad observationes Pachymerianas specimen sapientiae Indorum veterum liber olim ex lingua Indica in Persicam a Perzoe Medico, ex Persica in Arabicam ab Anonymo, ex Arabica in Graecam a Symeone Seth, a Petro Possino Societ. Jesu novissime e Graeca in Latinam translatus.
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Incluye: Jacobi Gretseri Societatis Jesu annotationes in Cantacuzeni historiam ; Jacobi Pontani Societatis Jesu notae in Cantacuzeni historiam, quibus partim ratio conversionis redditur, partim loci obscuriores explanantur, & insigniores illustrantur.
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Incluye según índice: Chronici jussu Constantini Porphyrogenneti conscripti, a Leone Armenio usque ad Michaelem Theophili ; Idem Constantinus Porphyrogennetus de Basilii Imp. avi vita & rebus gestis ; Anonymus continuator Theophanis, a Leone Sapiente usque ad Romanum, Constantini Porphyrogenneti ; Orthodoxorum Invectiva adversus Iconomachos ; Joannis Jerosolymitani Narratio de Iconomachis ; Joannes Cameniata, & Demetrius Cydonius, de Excidio Thessalonicae ; Symeonis Magistri ac Logothetae Annales, a Leone Armenio usque ad Nicephorum Phocam ; Georgii Monachi vitae recentiorum Imperatorum, a Leone Armenio usque ad Constantinum Porphyrogennetum.
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Mode of access: Internet.
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Mode of access: Internet.
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... El Discreto. Oráculo manual y arte de prudencia. El héroe / Baltasar Gracian.
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Incluye: Aeneae Sylvii Senensis, sive Pii Papae II, Historia Austriaca Friderici III Imperatoris.
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Mode of access: Internet.
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Several landforms found in the fold-and-thrust belt area of Central Precordillera, Pre-Andes of Argentina, which were often associated with tectonic efforts, are in fact related to non-tectonic processes or gravitational superficial structures. These second-order structures, interpreted as gravitational collapse structures, have developed in the western flank of sierras de La Dehesa and Talacasto. These include rock-slides, rock falls, wrinkle folds, slip sheets and flaps, among others; which together constitute a monoclinal fold dipping between 30º and 60º to the west. Gravity collapse structures are parallel to the regional strike of the Sierra de la Dehesa and are placed in Ordovician limestones and dolomites. Their sloping towards the west, the presence of bed planes, fractures and joints; and the lithology (limestone interbedded with incompetent argillaceous banks) would have favored their occurrence. Movement of the detached structures has been controlled by lithology characteristics, as well as by bedding and joints. Detachment and initial transport of gravity collapse structures and rockslides in the western flank of the Sierra de la Dehesa were tightly controlled by three structural elements: 1) sliding surfaces developed on parallel bedded strata when dipping >30° in the slope direction; 2) Joint’s sets constitute lateral and transverse traction cracks which release extensional stresses and 3) Discontinuities fragmenting sliding surfaces. Some other factors that could be characterized as local (lithology, structure and topography) and as regional (high seismic activity and possibly wetter conditions during the postglacial period) were determining in favoring the steady loss of the western mountain side in the easternmost foothills of Central Precordillera.