Relevant bibliographies by topics / North Alpine domain

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  1. Journal articles
  2. Dissertations / Theses
  3. Book chapters

Academic literature on the topic 'North Alpine domain'

Author: Grafiati
Published: 2 June 2025
Last updated: 31 July 2025

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Journal articles on the topic "North Alpine domain"

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Sissingh, W. "Kinematic sequence stratigraphy of the European Cenozoic Rift System and Alpine Foreland Basin: correlation with Mediterranean and Atlantic plate-boundary events." Netherlands Journal of Geosciences 85, no. 2 (2006): 77–129. http://dx.doi.org/10.1017/s0016774600077921.

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AbstractA review of the sequence stratigraphic development of the Tertiary basins of the North and West Alpine Foreland domains shows that their structural and depositional history was episodically affected by brief tectonic phases. These were associated with intermittent deformation events induced by the collisional convergence and compressional coupling of the Apulian and Iberian microplates with the European Plate. The plate kinematics-related episodicity was essentially isochronously recorded in the basin fills of the Alpine Foreland region. These are generally correlative with changes in
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Verwater, Vincent F., Eline Le Breton, Mark R. Handy, Vincenzo Picotti, Azam Jozi Najafabadi, and Christian Haberland. "Neogene kinematics of the Giudicarie Belt and eastern Southern Alpine orogenic front (northern Italy)." Solid Earth 12, no. 6 (2021): 1309–34. http://dx.doi.org/10.5194/se-12-1309-2021.

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Abstract. Neogene indentation of the Adriatic plate into Europe led to major modifications of the Alpine orogenic structures and style of deformation in the Eastern and Southern Alps. The Giudicarie Belt is a prime example of this, as it offsets the entire Alpine orogenic edifice; its activity has been kinematically linked to strike-slip faulting and lateral extrusion of the Eastern Alps. Remaining questions on the exact role of this fold-and-thrust belt in the structure of the Alpine orogen at depth necessitate a quantitative analysis of the shortening, kinematics, and depth of decoupling ben
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Casciello, Emilio, Manuel Fernàndez, Jaume Vergés, Massimo Cesarano, and Montserrat Torne. "The Alboran domain in the western Mediterranean evolution: the birth of a concept." Bulletin de la Société Géologique de France 186, no. 4-5 (2015): 371–84. http://dx.doi.org/10.2113/gssgfbull.186.4-5.371.

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Abstract Since the early 70’s the majority of tectonic reconstructions of the western Mediterranean employ the Alboran domain notion as a migrating microcontinent or landmass mainly composed of Paleozoic-Triassic rocks affected by ‘Alpine’ HP-LT metamorphism. For nearly three decades, since the mid-80’s, the Alboran domain was considered as a fragment of the Alpine chain that moved westward, colliding into Iberia and North Africa to produce the Gibraltar arc and Betic-Rif chain. In 2012, a new hypothesis for the evolution of the western Mediterranean was presented in which the Betic-Rif orogen
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Dannowski, Anke, Heidrun Kopp, Ingo Grevemeyer, et al. "Seismic evidence for failed rifting in the Ligurian Basin, Western Alpine domain." Solid Earth 11, no. 3 (2020): 873–87. http://dx.doi.org/10.5194/se-11-873-2020.

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Abstract. The Ligurian Basin is located in the Mediterranean Sea to the north-west of Corsica at the transition from the Western Alpine orogen to the Apennine system and was generated by the south-eastward trench retreat of the Apennines–Calabrian subduction zone. Late-Oligocene-to-Miocene rifting caused continental extension and subsidence, leading to the opening of the basin. Yet it remains unclear if rifting caused continental break-up and seafloor spreading. To reveal its lithospheric architecture, we acquired a 130 km long seismic refraction and wide-angle reflection profile in the Liguri
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Kováč, Michal, Emő Márton, Tomáš Klučiar, and Rastislav Vojtko. "Miocene basin opening in relation to the north-eastward tectonic extrusion of the ALCAPA Mega-Unit." Geologica Carpathica 69, no. 3 (2018): 254–63. http://dx.doi.org/10.1515/geoca-2018-0015.

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AbstractThe opening and evolution of the Western Carpathians Miocene basins was closely related to the north-eastward tectonic extrusion of the ALCAPA Mega-Unit lithosphere caused by the final stage of collision of the Eastern Alpine–Western Carpathian orogenic system with the European Platform and Alpine convergence with the Adria plate. The roll back effect of the oceanic or thinned continental crust of the Magura–Krosno realms, subduction below the front of the Carpathians in the north-east, east and relative plate velocities led to gradual stretching of the overriding micro-plates (defined
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Makris, J. "GEOPHYSICAL STUDIES AND TECTONISM OF THE HELLENIDES." Bulletin of the Geological Society of Greece 43, no. 1 (2017): 32. http://dx.doi.org/10.12681/bgsg.11158.

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By constraining gravity modelling by Deep Seismic Soundings (DSS) and the Bouguer gravity field of Greece a 3-D density-velocity model of the crust and upper mantle was developed. It was shown that in the north Aegean Trough and the Thermaikos Basins the sediments exceed 7 km in thickness. The basins along the western Hellenides and the coastal regions of western Greece are filled with sediments of up to 10 km thickness, including the Prepulia and Alpine metamorphic limestones. The thickest sedimentary series however, were mapped offshore southwest and southeast of Crete and are of the order o
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Haas, J., S. Kovács, L. Krystyn, and R. Lein. "Significance of Late Permian-Triassic facies zones in terrane reconstructions in the Alpine-North Pannonian domain." Tectonophysics 242, no. 1-2 (1995): 19–40. http://dx.doi.org/10.1016/0040-1951(94)00157-5.

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Alonso-Chaves, F., J. I. Soto, M. Orozco, A. A. Kilias, and M. D. Tranos. "TECTONIC EVOLUTION OF THE BETIC CORDILLERA: AN OVERVIEW." Bulletin of the Geological Society of Greece 36, no. 4 (2004): 1598. http://dx.doi.org/10.12681/bgsg.16563.

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The Betic (Southern Spain) and the Rif (Morocco) mountain chains, connected through the Gibraltar Strait, shapes a W-E elongated and arcuate Alpine orogenic belt. The Alborân Sea, in continuity to the east with the South Balearic Basin, is located in the inner part of this alpine belt. The Iberian and African continental forelands bound the region as a whole to the north and south, respectively, and to the east it is connected to the oceanic Sardine-Balearic Basin. The peculiarities of these westernmost Mediterranean chains result from: (1) its position between two large convergent plates -Afr
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Scapozza, Cristian, Chantal Del Siro, Christophe Lambiel, and Christian Ambrosi. "Schmidt hammer exposure-age dating of periglacial and glacial landforms in the Southern Swiss Alps based on <i>R</i>-value calibration using historical data." Geographica Helvetica 76, no. 4 (2021): 401–23. http://dx.doi.org/10.5194/gh-76-401-2021.

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Abstract. As a contribution to the palaeoenvironmental history reconstruction of the Alpine periglacial domain, this study focuses on the Schmidt hammer exposure-age dating (SHD) of (peri-)glacial landforms using rebound-value (R-value) calibrations for 10 stations in the Scaradra glacier forefield (north-eastern part of the Ticino Canton, Lepontine Alps) and for 13 stations in the Splügenpass region (located between Switzerland and Italy, Rhaetian Alps). Linear calibration based on the known age of several moraines of the Scaradra glacier assessed by historical cartography allowed the reconst
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Zouhri, Lahcen, Christian Lamouroux, Daniel Vachard, and Alain Pique. "Evidence of flexural extension of the Rif foreland: The Rharb-Mamora basin (northern Morocco)." Bulletin de la Société Géologique de France 173, no. 6 (2002): 509–14. http://dx.doi.org/10.2113/173.6.509.

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Abstract The Rharb-Mamora basin is the foreland of the Rif Cordillera (orogenic belt). The Mamora area (northern Morocco) is located at the southern border of the Rharb basin and intercalated between the Alpine Rif Mountains to the north and the Hercynian Moroccan Meseta domain to the south. Analysis and interpretation of seismic lines, hydrogeological and oil wells, have allowed to precise the major structural elements of the Mamora area, which is covered by late Neogene sediments. The structure of the area is controlled by faults that also affect the Paleozoic basement. The NE-SW and NW-SE t
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Dissertations / Theses on the topic "North Alpine domain"

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Ouazzani-Touhami, Mohamed. "Structures et recristallisations associees dans des zones de cisaillement : nappes de mascate (oman) et nappes de frederico s.l. (rif interne, maroc)." Université Louis Pasteur (Strasbourg) (1971-2008), 1986. http://www.theses.fr/1986STR13198.

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L'etude de la deformation et des recristallisations associees dans deux ensembles de nappes synmetamorphiques (mascate, oman; rif, maroc) a abouti a montrer que, dans les deux exemples, il apparait que les isogrades du metamorphisme sont perturbes par des chevauchements tardi- a post-metamorphiques, qui jouent un role important dans les dernieres phases de l'evolution thermique des piles tectoniques considerees. Les nappes de mascate (oman) representent un element tres interne, en fenetre, sous les nappes oceaniques chainees sur la plateforme arabe. En ce qui concerne les nappes de federico (r
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Book chapters on the topic "North Alpine domain"

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Gravela, Marta. "Prima dei Tuchini. Fedeltà di parte e comunità nelle valli del Canavese (Piemonte, secolo XIV)." In La signoria rurale nell’Italia del tardo medioevo. 3 L’azione politica locale. Firenze University Press, 2021. http://dx.doi.org/10.36253/978-88-5518-427-4.03.

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Famous for the late 14th-century revolt known as Tuchinaggio, the Canavese area, in north-western Piedmont, provides significant information concerning the relationship between lords and subjects in a longer time span. By analysing a wide range of sources (pastoral visitations, chronicles, court and notarial records, statutes), the essay examines the domini-homines dialectic in the first half of the 14th century: in the Canavese Alpine valleys various degrees of institutional consolidation of communities can be outlined, identifying a process of growth common to communities in the entire Alpin
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Alexander, Earl B., Roger G. Coleman, Todd Keeler-Wolfe, and Susan P. Harrison. "Gulf of Alaska, Domain 8." In Serpentine Geoecology of Western North America. Oxford University Press, 2007. http://dx.doi.org/10.1093/oso/9780195165081.003.0026.

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The Gulf of Alaska domain extends eastward from Kodiak Island across the Kenai Peninsula, around the Chugach Mountains, and beyond Tonsina, curves southward across the glacier-covered St. Elias Mountains. The southeastern segment of the domain is west of the Canadian Coastal Mountains and includes the coastline and islands in southeastern Alaska. Ultramafic rocks occur sporadically in this region from British Columbia northwestward through southeastern Alaska and around the Gulf of Alaska to the Kenai Peninsula. Most of this domain is mountainous, especially in areas where there are ultramafic
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Alexander, Earl B., Roger G. Coleman, Todd Keeler-Wolfe, and Susan P. Harrison. "Northern Cascade-Fraser River, Domain 7." In Serpentine Geoecology of Western North America. Oxford University Press, 2007. http://dx.doi.org/10.1093/oso/9780195165081.003.0025.

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The Northern Cascade–Fraser River domain conforms to the Northern Cascade Mountains physiographic province in northwestern Washington and southern British Columbia, the San Juan Islands between the southern tip of Vancouver Island and the Northern Cascade Mountains, and much of the Interior Plateau province of British Columbia. The thread that connects these areas is the north–south Straight Creek–Fraser River fault system that runs through the Northern Cascade Mountains and northward along the Fraser River. The localities of domain 7 are along faults that branch off from this major fault syst
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Demoulin, Alain. "Tectonic Evolution, Geology, and Geomorphology." In The Physical Geography of Western Europe. Oxford University Press, 2005. http://dx.doi.org/10.1093/oso/9780199277759.003.0010.

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The present-day major relief features of western Europe are to a great extent determined by the underlying geological structures, either passively or actively. To get a comprehensive picture of their morphological evolution and interrelations, this chapter provides an overview of the spatial and temporal characteristics of the larg-escale tectonic framework of the continent. After having described the west European landscape at the end of the Palaeozoic, to which time the oldest preserved landforms date back, an outline of the Mesozoic and Cenozoic history of the major tectonic domains follows
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