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Готові списки джерел за темами / Balearic promontory / Статті в журналах

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Статті в журналах з теми "Balearic promontory"

Автор: Grafiati

Опубліковано: 1 лютого 2023

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1

Anglada, Montserrat, Antoni Ferrer, Damià Ramis, Magdalena Salas, Mark Van Strydonck, Maria José León, and Lluís Plantalamor. "Dating Prehistoric Fortified Coastal Sites in the Balearic Islands." Radiocarbon 59, no. 5 (September 18, 2017): 1251–62. http://dx.doi.org/10.1017/rdc.2017.51.

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AbstractA special type of coastal settlement, promontory forts defended by inland-facing walls, appeared in the Balearic Islands in an imprecise time during the Bronze Age. A research project was initiated in 2011 to study one of these sites on each of the two major islands of the archipelago. The first one, Es Coll de Cala Morell (north Menorca), is a walled promontory with a relatively large plateau, with 13 horseshoe-shaped houses (navetes). The second, Sa Ferradura (east Mallorca), is a smaller coastal cape, with a different spatial planning, with only two large built-up areas, both attached to the enclosure wall. Two of the navetes have been excavated at Es Coll de Cala Morell, showing a domestic space with a central hearth in both cases. The occupation has been dated to around 1600–1200 cal BC. At Sa Ferradura seven hearths have been recorded in a large, open-air area. Their chronology falls within the interval of approximately 1200/1100–900 cal BC. From a chronological point of view, fortified settlements in coastal promontories are not, as was expected, a unitary phenomenon in Menorca and Mallorca and have to be related to different cultural periods.

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2

Acosta, Juan, Miquel Canals, Jerónimo López-Martı́nez, Araceli Muñoz, Pedro Herranz, Roger Urgeles, Carlos Palomo, and Jose L. Casamor. "The Balearic Promontory geomorphology (western Mediterranean): morphostructure and active processes." Geomorphology 49, no. 3-4 (January 2003): 177–204. http://dx.doi.org/10.1016/s0169-555x(02)00168-x.

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3

Acosta, J., A. Muñoz, P. Herranz, C. Palomo, M. Ballesteros, M. Vaquero, and E. Uchupi. "Geodynamics of the Emile Baudot Escarpment and the Balearic Promontory, western Mediterranean." Marine and Petroleum Geology 18, no. 3 (March 2001): 349–69. http://dx.doi.org/10.1016/s0264-8172(01)00003-4.

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4

Acosta, J., E. Ancochea, M. Canals, M. J. Huertas, and E. Uchupi. "Early Pleistocene volcanism in the Emile Baudot Seamount, Balearic Promontory (western Mediterranean Sea)." Marine Geology 207, no. 1-4 (June 2004): 247–57. http://dx.doi.org/10.1016/j.margeo.2004.04.003.

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5

Maillard, Agnès, Olivier Driussi, Johanna Lofi, Anne Briais, Franck Chanier, Christian Hübscher, and Virginie Gaullier. "Record of the Messinian Salinity Crisis in the SW Mallorca area (Balearic Promontory, Spain)." Marine Geology 357 (November 2014): 304–20. http://dx.doi.org/10.1016/j.margeo.2014.10.001.

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6

Maillard, Agnès, Fadl Raad, Frank Chanier, Hanneke Heida, Johanna Lofi, Guillem Mas, and Daniel Garcia-Castellanos. "Plio-Quaternary strike-slip tectonics in the Central Mallorca Depression, Balearic Promontory: Land–sea correlation." Tectonophysics 829 (April 2022): 229295. http://dx.doi.org/10.1016/j.tecto.2022.229295.

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7

Driussi, Olivier, Agnès Maillard, Diana Ochoa, Johanna Lofi, Franck Chanier, Virginie Gaullier, Anne Briais, Françoise Sage, Francisco Sierro, and Marga Garcia. "Messinian Salinity Crisis deposits widespread over the Balearic Promontory: Insights from new high-resolution seismic data." Marine and Petroleum Geology 66 (September 2015): 41–54. http://dx.doi.org/10.1016/j.marpetgeo.2014.09.008.

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8

Driussi, Olivier, Anne Briais, and Agnès Maillard. "Evidence for transform motion along the South Balearic margin and implications for the kinematics of opening of the Algerian basin." Bulletin de la Société Géologique de France 186, no. 4-5 (July 1, 2015): 353–70. http://dx.doi.org/10.2113/gssgfbull.186.4-5.353.

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Abstract Two major types of kinematic models have been proposed to explain the opening of the western Mediterranean basins (Liguro-Provençal and Algerian basins, and Valencia trough). In one type of models, all continental blocks bounding the basins drift to the southeast, driven by the rollback of the Tethys subduction slab. In the other type of models, the Alboran domain drifts to the southwest, implying a westward rollback of the broken subducting slab and a NE-SW opening of the Algerian basin. In most models, however, the structure of the Balearic promontory was not taken into account, despite its key location at the boundary of the three major basins. We used the interpretation of a large seismic database coupled to gravity and magnetic anomaly analyses to characterize the nature and structure of the South Balearic margin. The constraints brought by the new analyses allow us to suggest a new scenario for the opening of the Algerian basin. Seismic profiles show that the South Balearic margin is composed of four segments with different morphologies and crustal structures. Two segments, the Mazarron and the Emile Baudot escarpments, are characterized by steep scarps and sharp crustal thinning. Two other segments, the South Ibiza and South Menorca margins, have a smoother bathymetry and crustal thinning. We interpret the former in terms of transform margins, and the latter as divergent margins. The distribution of faults on the passive margin segments suggests that they have recorded at least two phases of deformation. A first phase of opening, probably in a NW-SE direction, affected the south Balearic margin, and possibly created some oceanic floor. The existence of the transform margin segments and the prominent NW-SE orientation of the magnetic lineations in the eastern Algerian basin suggest that most of this basin opened in a NE-SW direction, in different oceanic corridors. The two eastern corridors formed by the southwestward drift of the Kabylies. The western corridor, bounded by the transform segments of the South Balearic margin and the Algerian margin, results from the southwestward drift of the Alboran domain, as suggested by previous studies.

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9

Depalmas, Anna. "New Data from Fortified Coastal Settlement of Cap de Forma, Mahon, Menorca (Balearic Islands)." Radiocarbon 56, no. 2 (2014): 425–37. http://dx.doi.org/10.2458/56.17169.

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This article presents new radiometric data from archaeological layers of the inhabited structures adjacent to the cyclopean monument of Cap de Forma (Mahon, Menorca). The archaeological site is located on a narrow isthmus that links a 30-m-high coastal promontory to the mainland. It is next to an excellent natural harbor on the south coast of the island. The protohistorical complex consists of a cyclopean monument surrounded by a necropolis of rock-cut tombs (cuevas) that are dug into the cliff. The monument is an atypical example of Talayotic architecture. The excavations carried out since 1997 have discovered three living spaces. These lean against the southern wall of the cyclopean structure. The artifacts are almost all pan of a chronological horizon that corresponds to the beginning of the Talayotic period. This study uses radiometric data to help interpret the recent findings from the three living spaces that flank the wall of the central monument.

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10

Depalmas, Anna. "New Data from Fortified Coastal Settlement of Cap de Forma, Mahon, Menorca (Balearic Islands)." Radiocarbon 56, no. 02 (2014): 425–37. http://dx.doi.org/10.1017/s0033822200049481.

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Анотація:

This article presents new radiometric data from archaeological layers of the inhabited structures adjacent to the cyclopean monument of Cap de Forma (Mahon, Menorca). The archaeological site is located on a narrow isthmus that links a 30-m-high coastal promontory to the mainland. It is next to an excellent natural harbor on the south coast of the island. The protohistorical complex consists of a cyclopean monument surrounded by a necropolis of rock-cut tombs (cuevas) that are dug into the cliff. The monument is an atypical example of Talayotic architecture. The excavations carried out since 1997 have discovered three living spaces. These lean against the southern wall of the cyclopean structure. The artifacts are almost all pan of a chronological horizon that corresponds to the beginning of the Talayotic period. This study uses radiometric data to help interpret the recent findings from the three living spaces that flank the wall of the central monument.

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11

Raad, Fadl, Johanna Lofi, Agnès Maillard, Athina Tzevahirtzian, and Antonio Caruso. "The Messinian Salinity Crisis deposits in the Balearic Promontory: An undeformed analog of the MSC Sicilian basins??" Marine and Petroleum Geology 124 (February 2021): 104777. http://dx.doi.org/10.1016/j.marpetgeo.2020.104777.

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12

J., Acosta, Muñoz A., Herranz P., Palomo C., Ballesteros M., Vaquero M., and Uchupi E. "Pockmarks in the Ibiza Channel and western end of the Balearic Promontory (western Mediterranean) revealed by multibeam mapping." Geo-Marine Letters 21, no. 3 (November 1, 2001): 123–30. http://dx.doi.org/10.1007/s003670100074.

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13

Etheve, Nathalie, Dominique Frizon de Lamotte, Geoffroy Mohn, Raquel Martos, Eduard Roca, and Christian Blanpied. "Extensional vs contractional Cenozoic deformation in Ibiza (Balearic Promontory, Spain): Integration in the West Mediterranean back-arc setting." Tectonophysics 682 (July 2016): 35–55. http://dx.doi.org/10.1016/j.tecto.2016.05.037.

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14

Maillard, Agnès, Virginie Gaullier, Carine Lézin, Frank Chanier, Francis Odonne, and Johanna Lofi. "New onshore/offshore evidence of the Messinian Erosion Surface from key areas: The Ibiza-Balearic Promontory and the Orosei-Eastern Sardinian margin." BSGF - Earth Sciences Bulletin 191 (2020): 9. http://dx.doi.org/10.1051/bsgf/2020007.

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As the Messinian sea-level draw down associated with the Messinian Salinity Crisis is still questioned, we propose to show that the widely spread erosion surface affecting the Mediterranean margins is indeed linked to an exondation demonstrated from offshore and onshore data. Our study presents a comprehensive onshore to offshore correlation of the Messinian erosional surface. It is focused on small drainage systems or interfluve areas, outside of evaporite basins or incised canyons, where the Messinian erosion had not yet been studied previously: around Ibiza on the Balearic Promontory and around Orosei on the Eastern Sardinian margin, Tyrrhenian Basin, both areas where new offshore data were recently acquired. We show that the late Messinian erosion formed in subaerial settings, as testified by evidence of continentalization events, and attests for a regression phase that was correlated from the offshore continental slopes to the onshore paleo-platforms in both areas. Characteristics of this erosion in both study areas strengthen the scenario with at least one important low-stand sea-level for the Messinian Salinity Crisis with evaporites subbasins lying at different depths and possibly disconnected.

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15

Kaminski, Pauline, Thore Sager, Jürgen Grabe, and Morelia Urlaub. "A new methodology to assess the potential of conjectural trigger mechanisms of submarine landslides exemplified by marine gas occurrence on the Balearic Promontory." Engineering Geology 295 (December 2021): 106446. http://dx.doi.org/10.1016/j.enggeo.2021.106446.

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16

Viti, Marcello, Enzo Mantovani, Daniele Babbucci, Caterina Tamburelli, Marcello Caggiati, and Alberto Riva. "Basic Role of Extrusion Processes in the Late Cenozoic Evolution of the Western and Central Mediterranean Belts." Geosciences 11, no. 12 (December 7, 2021): 499. http://dx.doi.org/10.3390/geosciences11120499.

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Tectonic activity in the Mediterranean area (involving migrations of old orogenic belts, formation of basins and building of orogenic systems) has been determined by the convergence of the confining plates (Nubia, Arabia and Eurasia). Such convergence has been mainly accommodated by the consumption of oceanic and thinned continental domains, triggered by the lateral escapes of orogenic wedges. Here, we argue that the implications of the above basic concepts can allow plausible explanations for the very complex time-space distribution of tectonic processes in the study area, with particular regard to the development of Trench-Arc-Back Arc systems. In the late Oligocene and lower–middle Miocene, the consumption of the eastern Alpine Tethys oceanic domain was caused by the eastward to SE ward migration/bending of the Alpine–Iberian belt, driven by the Nubia–Eurasia convergence. The crustal stretching that developed in the wake of that migrating Arc led to formation of the Balearic basin, whereas accretionary activity along the trench zone formed the Apennine belt. Since the collision of the Anatolian–Aegean–Pelagonian system (extruding westward in response to the indentation of the Arabian promontory) with the Nubia-Adriatic continental domain, around the late Miocene–early Pliocene, the tectonic setting in the central Mediterranean area underwent a major reorganization, aimed at activating a less resisted shortening pattern, which led to the consumption of the remnant oceanic and thinned continental domains in the central Mediterranean area.

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17

Cartes, J. E., D. Díaz-Viñolas, V. Papiol, A. Lombarte, A. Serrano, A. Carbonell, C. Salas, et al. "First faunistic results on Valencia (Cresques) Seamount, with some ecological considerations." Marine Biodiversity Records 14, no. 1 (September 7, 2021). http://dx.doi.org/10.1186/s41200-021-00210-y.

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AbstractThe living and dead fauna of Valencia Seamount, a deep promontory in the middle of the Balearic Basin which summit is at ca. 1100 m depth, is described by first time based in a rock dredge perfomed in a sedimentary area of the summit Mount. Surface-feeder polychaetes (the Paraonidae Levinsenia gracilis and Terebellidae as dominant), and taxodont bivalves (Ledella messanensis and Yoldiella ovulum) were the main species of benthos. We found alive remains of the bamboo coral Isidella elongata, a vulnerable, habitat-forming species in the deep Mediterranean. Benthos density was low (0.6 organisms/2 dm3 mud). Thanatocoenosis evidenced a rather moderate diversity of benthic bivalves (11 species) and gastropods (9 species) also dominated by surface deposit feeders. Fish (identified/quantified from sedimented otoliths) showed diversified and abundant mesopelagic fauna, mainly Myctophidae. More interestingly, we highlighted among benthopelagic fish the occurrence of recruits of Merluccius merluccius, Micromesistius poutassou, or Hymenocephalus italicus, all species that live in the neighboring slopes of the Iberian Peninsula and the Balearic Islands at quite shallower depths (at 100-700 m) than their distribution in the Valencia Seamount summit (1102–1130 m) based on the deposited otoliths found. Some ecological aspects were discussed and the necessity to consider the deep Valencia Seamount as a potential area that should be under protection.

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18

Raad, Fadl, Ronja Ebner, Hanneke Heida, Paul Meijer, Johanna Lofi, Agnès Maillard, and Daniel Garcia‐Castellanos. "A song of volumes, surfaces and fluxes – The case study of the Central Mallorca Depression (Balearic Promontory) during the Messinian Salinity Crisis." Basin Research, August 11, 2022. http://dx.doi.org/10.1111/bre.12702.

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19

Bravo Asensio, Cristina, Irene Riudavets González, and Gerard Remolins Zamora. "A proposal for the study of coastal Roman Late Republican sites on Menorca (Balearic Islands) from the case of Mongofre Nou." BSAA arqueología, February 18, 2021, 48–75. http://dx.doi.org/10.24197/ba.0.2020.48-75.

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El presente trabajo expone una propuesta para el estudio de los yacimientos costeros de época tardorrepublicana en la isla de Menorca (Islas Baleares), con el objeto de estudiar y comprobar la hipótesis que sostienen los autores sobre la existencia de una serie de puestos de vigilancia de la costa por parte del ejército romano durante y después de la conquista de las Baleares (123 – 121 a.C.). Este proyecto en curso y de largo recorrido, cuyas características principales se describen en las siguientes páginas, ha incluido, hasta la fecha, la prospección sistemática y excavación de un yacimiento arqueológico localizado sobre un promontorio costero al noreste de la isla (Mongofre Nou, Maó), los resultados del cual se presentan aquí.

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