2026-04-29T09:32:29Zhttps://riubu.ubu.es/oai/request

oai:riubu.ubu.es:10259/86222024-02-08T01:05:33Zcom_10259_7396com_10259.4_2505com_10259.4_106com_10259_2604col_10259_7397

Ortega, Ana Isabel b61652cd-f5e3-46e7-b906-1247a550bdf3 600 Benito Calvo, Alfonso ca2bdd5a-6d7b-4f67-a8f8-0d46b88cc9d3 600 Porres Benito, José Ángel 450 600 Pérez González, Alfredo 5d8d0f42-147a-49ac-b640-ad89750ed6c6 600 Martín Merino, Miguel Ángel 065f72e6-0779-4c4d-9c39-a9ed46cad5e9 600 2024-02-07T13:27:03Z 2024-02-07T13:27:03Z 2010-10 1075-2196 http://hdl.handle.net/10259/8622 10.1002/arp.392 1099-0763 In this paper we have applied the electrical resistivity tomography (ERT) in order to prospect and to analyse the morphological and geological subsurface of the Torcas-Cueva Mayor endokarst system (Sierra de Atapuerca). These works are essential to establish the development of the sedimentary infills where the Early and Middle Pleistocene archaeo-palaeoanthropological sites of the Sierra de Atapuerca are located. The prospecting was based on the elaboration of 15 ERT sections, which were interpreted using topographic, archaeological, geological and geomorphological data. Through this procedure we have indentified the endokarst morphologies and the main lithological groups. The latter correspond to the Upper Cretaceous limestones and dolostones (> 1500 ohm m−1) and Neogene sediments and Quaternary valley infills (< 400 ohm m−1). The endokarst structures inside the Upper Cretaceous carbonates were related to empty cavities (> 1500 ohm m−1), passages filled with speleothems (400–1500 ohm m−1and with detrital materials (< 400 ohm m−1), such as the deposits of the Dolina, Elefante and Galería sites. The analysis of these subsurface structures shows that the karstic passages present a regular south–north development, starting with subsurface faults detected in the north margin of the main valley (Arlanzón River) and finishing along the Pico valley headwaters. These passages were cut off by the Pleistocene incision of the Sierra de Atapuerca minor valleys (e.g. Propiedad valley), forming entrances to caves that were occupied by hominids and fauna from Early Pleistocene times. This work was supported by the research projects BXX2000-1258-03-02, BOSS2003-08938-C03-01 and CGL2006-13532-C03-02 of the Dirección General de Investigación Científica y Técnica (DGICYT), and by the Junta de Castilla y León. application/pdf eng Wiley Archaeological Prospection. 2010, V. 17, n. 4, p. 233-245 https://doi.org/10.1002/arp.392 Electrical resistivity tomography Cave Geoarchaeological prospection Sierra de Atapuerca sites Schlumberger-Wenner geolectric Dipole-dipole geolectric Geología Arqueología-Burgos Geology Archaeology-Burgos Applying electrical resistivity tomography to the identification of endokarstic geometries in the Pleistocene Sites of the Sierra de Atapuerca (Burgos, Spain) info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion info:eu-repo/semantics/closedAccess Archaeological Prospection 17 4 233 245 THUMBNAIL Ortega-ap_2010.pdf.jpg Ortega-ap_2010.pdf.jpg IM Thumbnail image/jpeg 4526 https://riubu.ubu.es/bitstream/10259/8622/3/Ortega-ap_2010.pdf.jpg f3baac7c57579d0768d88daa1e326692 MD5 3 LICENSE license.txt license.txt text/plain; charset=utf-8 1362 https://riubu.ubu.es/bitstream/10259/8622/2/license.txt 5d013bfa6e473ff0db22cd82a4d71a70 MD5 2 ORIGINAL Ortega-ap_2010.pdf Ortega-ap_2010.pdf Archivo cerrado application/pdf 714778 https://riubu.ubu.es/bitstream/10259/8622/1/Ortega-ap_2010.pdf 6def743d289e192aa1a60d1582b780bf MD5 1 10259/8622 oai:riubu.ubu.es:10259/8622 2024-02-08 02:05:33.353 Repositorio Institucional de la Universidad de Burgos bubrep@ubu.es RWwgYXV0b3IgY29tbyDDum5pY28gdGl0dWxhciBkZSBsb3MgZGVyZWNob3MgZGUgcHJvcGllZGFkIGludGVsZWN0dWFsIGRlIGxhIG9icmEsIG8gZGlzcG9uaWVuZG8gZGUgbG9zIGRlYmlkb3MgcGVybWlzb3MgZGUgbG9zIG90cm9zIHRpdHVsYXJlcywgc2kgbG9zIGh1YmllcmEsIHkgZW4gdmlydHVkIGRlIGxvcyBkZXJlY2hvcyBxdWUgbGUgY29uZmllcmUgbGEgbGVnaXNsYWNpw7NuIHZpZ2VudGUgc29icmUgcHJvcGllZGFkIGludGVsZWN0dWFsIHkgZGVyZWNob3MgZGUgYXV0b3IsIApBVVRPUklaQSBhIGxhIFVuaXZlcnNpZGFkIGRlIEJ1cmdvcyBhIGRpZnVuZGlyLCBkZSBtYW5lcmEgZ3JhdHVpdGEsIGVsIGNvbnRlbmlkbyBkZSBsb3MgYXJjaGl2b3MgZGlnaXRhbGVzIHF1ZSBjb3JyZXNwb25kZW4gYWwgZG9jdW1lbnRvIGRlc2NyaXRvIGFudGVyaW9ybWVudGUsIGNvbiBjYXLDoWN0ZXIgbm8gZXhjbHVzaXZvIHkgZGUgbWFuZXJhIHDDumJsaWNhIGVuIGFjY2VzbyBhYmllcnRvIGEgdHJhdsOpcyBkZSBJbnRlcm5ldCwgcGFyYSBsbyBxdWUgbGEgQmlibGlvdGVjYSBwcm9jZWRlcsOhIGEgYXJjaGl2YXJsb3MgZW4gZWwgUmVwb3NpdG9yaW8gSW5zdGl0dWNpb25hbC4gQXNpbWlzbW8gYXV0b3JpemEgYSBsYSBVbml2ZXJzaWRhZCBkZSBCdXJnb3MgYSByZWFsaXphciBsYXMgdHJhbnNmb3JtYWNpb25lcyBuZWNlc2FyaWFzIGRlIGZvcm1hdG8sIG5vIGRlIGNvbnRlbmlkbywgcGFyYSBnYXJhbnRpemFyIGxhIHByZXNlcnZhY2nDs24geSBlbCBhY2Nlc28gZW4gZWwgZnV0dXJvLgoKRWwgYXV0b3IgZGlzcG9uZSwgZW4gdG9kbyBjYXNvLCBkZWwgZGVyZWNobyBhIHJldm9jYXIgZXN0YSBhdXRvcml6YWNpw7NuLgoKTGEgY2VzacOzbiBkZSBkZXJlY2hvcyBkZSBlc3RhIG9icmEgc2UgZW5jdWVudHJhIHN1amV0YSBhIGxhIGxlZ2lzbGFjacOzbiB2aWdlbnRlIHNvYnJlIHByb3BpZWRhZCBpbnRlbGVjdHVhbCB5IGRlcmVjaG9zIGRlIGF1dG9yLiBTdSBkaWZ1c2nDs24gZW4gZWwgUmVwb3NpdG9yaW8gc2Vyw6EgYmFqbyBsYSBtb2RhbGlkYWQgZGUgbGljZW5jaWEgQ3JlYXRpdmUgQ29tbW9ucyBvIGVxdWl2YWxlbnRlOiByZWNvbm9jaW1pZW50byDigJMgdXNvIG5vIGNvbWVyY2lhbCDigJMgc2luIG9icmEgZGVyaXZhZGEsIHBvciBsYSBxdWUgc2UgcGVybWl0ZSBoYWNlciBjb3BpYSwgZGlzdHJpYnVpciB5IGNvbXVuaWNhciBww7pibGljYW1lbnRlIGxhIG9icmEgc2llbXByZSBxdWUgc2UgY2l0ZSBhbCBhdXRvciwgZWwgdXNvIHF1ZSBzZSBoYWdhIGRlIGVsbGEgc2VhIG5vIGNvbWVyY2lhbCB5IG5vIHNlIGNyZWVuIG9icmFzIGRlcml2YWRhcyBhIHBhcnRpciBkZSBsYSBvcmlnaW5hbC4K