2D and 3D ERT imaging for identifying karst morphologies in the archaeological sites of Gran Dolina and Galeria Complex (Sierra de Atapuerca, Burgos, Spain)

被引：28

作者：

Bermejo, Lucia ^{[1
,2
,8
]}

Isabel Ortega, Ana ^{[1
,3
]}

Guerin, Roger ^{[4
]}

Benito-Calvo, Alfonso ^{[1
]}

Perez-Gonzalez, Alfredo ^{[1
]}

Pares, Josep M. ^{[1
]}

Aracil, Enrique ^{[5
]}

Bermudez de Castro, Jose Maria ^{[1
]}

Carbonell, Eudald ^{[6
,7
,8
]}

机构：

[1] Ctr Nacl Invest Evoluc Humana CENIEH, Paseo Sierra de Atapuerca 3, Burgos 09002, Spain

[2] Escuela Interuniv Posgrad Evoluc Humana, C Don Juan Austria 1, Burgos 09001, Spain

[3] Excma Diputac Prov Burgos, Grp Espeleol Edelweiss, C Paseo Espolon S-N, Burgos 09071, Spain

[4] UPMC Univ Paris 06, Sorbonne Univ, UMR 7619, METIS, F-75005 Paris, France

[5] Anal & Gest Subsuelo SL, C Luxemburgo 4,Portal 1,Oficina 3, Madrid 28224, Spain

[6] CSIC, Unidad Asociad, Inst Catala Paleoecol Humana & Evolucio Social, IPHES, C Escorxador S-N, Tarragona 43003, Spain

[7] Univ Rovira & Virgili, Campus Catalunya,Avinguda Catalunya 35, Tarragona 43002, Spain

[8] Equipo Invest Primeros Pobladores Extremadura, Casa Cultura Antonio Rodriguez Monino, Caceres 10003, Spain

来源：

QUATERNARY INTERNATIONAL | 2017年 / 433卷

关键词：

Electrical resistivity tomography; Cave; Geoarchaeological exploration; Sierra de Atapuerca sites; Karst geomorphology; ELECTRICAL-RESISTIVITY TOMOGRAPHY; PLEISTOCENE SITES; DC-RESISTIVITY; DE-ATAPUERCA; INVERSION; CAVES; ARRAY; RECONSTRUCTION; CHRONOLOGY; RESOLUTION;

D O I：

10.1016/j.quaint.2015.12.031

中图分类号：

P9 [自然地理学];

学科分类号：

0705 ; 070501 ;

摘要：

This work focusses on the Sierra de Atapuerca Thinchera karst system, in which Gran Dolina and Galeria Complex sites are located. A total of eight ERT profiles were performed over an area that covers both sites, with the aim of identifying the dimensions and continuity of these passages. The interpretation of the 2D and 3D profiles has allowed determining the extension of the conduits as well as the presence of a filled entrance that might be common to both sites. With the aid of 2D modelling experiments it was also possible to resolve some of the hypothesis raised from the interpretation of the 2D pseudosections. All these data have ultimately lead to a better understanding of the karst and sites' formation process. (C) 2015 Elsevier Ltd and INQUA. All rights reserved.

引用

页码：393 / 401

页数：9

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