FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2891957145> ?p ?o ?g. }

• W2891957145 endingPage "174" @default.
• W2891957145 startingPage "155" @default.
• W2891957145 abstract "Research Article| September 12, 2018 Sediment fill geometry and structural control of the Pampa del Tamarugal basin, northern Chile N. Labbé; N. Labbé † 1Advanced Mining Technology Center, Universidad de Chile, Avenida Tupper 2007, Santiago, Chile2Departamento de Geología, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Plaza Ercilla 803, Santiago, Chile †nlabbe@ing.uchile.cl Search for other works by this author on: GSW Google Scholar M. García; M. García 1Advanced Mining Technology Center, Universidad de Chile, Avenida Tupper 2007, Santiago, Chile2Departamento de Geología, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Plaza Ercilla 803, Santiago, Chile Search for other works by this author on: GSW Google Scholar Y. Simicic; Y. Simicic 1Advanced Mining Technology Center, Universidad de Chile, Avenida Tupper 2007, Santiago, Chile2Departamento de Geología, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Plaza Ercilla 803, Santiago, Chile Search for other works by this author on: GSW Google Scholar E. Contreras-Reyes; E. Contreras-Reyes 3Departamento de Geofísica, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Avenida Blanco Encalada 2002, Santiago, Chile Search for other works by this author on: GSW Google Scholar R. Charrier; R. Charrier 2Departamento de Geología, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Plaza Ercilla 803, Santiago, Chile4Escuela de Ciencias de la Tierra, Universidad Andres Bello, Sazié 2119, Santiago, Chile Search for other works by this author on: GSW Google Scholar G. De Pascale; G. De Pascale 2Departamento de Geología, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Plaza Ercilla 803, Santiago, Chile Search for other works by this author on: GSW Google Scholar C. Arriagada C. Arriagada 2Departamento de Geología, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Plaza Ercilla 803, Santiago, Chile Search for other works by this author on: GSW Google Scholar Author and Article Information N. Labbé † 1Advanced Mining Technology Center, Universidad de Chile, Avenida Tupper 2007, Santiago, Chile2Departamento de Geología, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Plaza Ercilla 803, Santiago, Chile M. García 1Advanced Mining Technology Center, Universidad de Chile, Avenida Tupper 2007, Santiago, Chile2Departamento de Geología, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Plaza Ercilla 803, Santiago, Chile Y. Simicic 1Advanced Mining Technology Center, Universidad de Chile, Avenida Tupper 2007, Santiago, Chile2Departamento de Geología, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Plaza Ercilla 803, Santiago, Chile E. Contreras-Reyes 3Departamento de Geofísica, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Avenida Blanco Encalada 2002, Santiago, Chile R. Charrier 2Departamento de Geología, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Plaza Ercilla 803, Santiago, Chile4Escuela de Ciencias de la Tierra, Universidad Andres Bello, Sazié 2119, Santiago, Chile G. De Pascale 2Departamento de Geología, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Plaza Ercilla 803, Santiago, Chile C. Arriagada 2Departamento de Geología, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Plaza Ercilla 803, Santiago, Chile †nlabbe@ing.uchile.cl Publisher: Geological Society of America Received: 07 Dec 2016 Revision Received: 27 Sep 2017 Accepted: 16 May 2018 First Online: 12 Sep 2018 Online Issn: 1943-2674 Print Issn: 0016-7606 © 2018 Geological Society of America GSA Bulletin (2019) 131 (1-2): 155–174. https://doi.org/10.1130/B31722.1 Article history Received: 07 Dec 2016 Revision Received: 27 Sep 2017 Accepted: 16 May 2018 First Online: 12 Sep 2018 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation N. Labbé, M. García, Y. Simicic, E. Contreras-Reyes, R. Charrier, G. De Pascale, C. Arriagada; Sediment fill geometry and structural control of the Pampa del Tamarugal basin, northern Chile. GSA Bulletin 2018;; 131 (1-2): 155–174. doi: https://doi.org/10.1130/B31722.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract Determination of the sediment fill geometry and structure of basins along the western flank of the Central Andes is crucial for understanding the regional tectonic evolution and the geological situation of natural resources. In this study, we developed a sediment-thickness distribution model for the Pampa del Tamarugal basin (between 20°20′S and 21°30′S, northern Chile), from surface geological information, available wells, and interpretation and depth conversion of 14 seismic-reflection profiles. Four Oligocene–Holocene units and one Carboniferous–Eocene undifferentiated basement unit were identified in the seismic profiles. For depth conversion, we established an empirical velocity model using P-wave velocities measured from rock samples, with velocity values from 2 to 6 km/s. By interpolating the basal-fill surface from the processed data set, and subtracting it from the topographic surface, we generated an isopach map of the basin, which has a maximum fill thickness of 1566 m. Four N-S–elongated asymmetric subbasins with a fill exceeding 700 m in thickness were identified, and these are separated by four basement highs. Both basement and fill units are folded and cut by west-vergent high-angle reverse faults, which originated before the Oligocene and were reactivated in the Miocene. During the isopach map construction, three sources of error were identified (i.e., topographic adjustment, interpretation, and conversion method), and the mean accumulated thickness error was found to be ±250 m; in addition, the lack of wells as validation data also contributes to the uncertainty. Based on our results, the basin-fill geometry was controlled by both compressional tectonics, which generated uplifted blocks and accommodation spaces, and desertification, which has significantly decreased the sediment input since the late Miocene. Despite the uncertainties, our results provide new insights into Andean tectonics and may be used as a screening tool for natural resources such as minerals and groundwater. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
• W2891957145 created "2018-09-27" @default.
• W2891957145 creator A5000154624 @default.
• W2891957145 creator A5009827828 @default.
• W2891957145 creator A5012112613 @default.
• W2891957145 creator A5021142496 @default.
• W2891957145 creator A5061081115 @default.
• W2891957145 creator A5068880809 @default.
• W2891957145 creator A5076447304 @default.
• W2891957145 date "2018-09-12" @default.
• W2891957145 modified "2023-10-02" @default.
• W2891957145 title "Sediment fill geometry and structural control of the Pampa del Tamarugal basin, northern Chile" @default.
• W2891957145 cites W1541615627 @default.
• W2891957145 cites W1586157160 @default.
• W2891957145 cites W1616442866 @default.
• W2891957145 cites W1624477729 @default.
• W2891957145 cites W1680466068 @default.
• W2891957145 cites W1868094023 @default.
• W2891957145 cites W1902436126 @default.
• W2891957145 cites W1921350963 @default.
• W2891957145 cites W1968126362 @default.
• W2891957145 cites W1970298434 @default.
• W2891957145 cites W1971007384 @default.
• W2891957145 cites W1984005435 @default.
• W2891957145 cites W1985930163 @default.
• W2891957145 cites W1986501104 @default.
• W2891957145 cites W1996730558 @default.
• W2891957145 cites W1996957031 @default.
• W2891957145 cites W1998282979 @default.
• W2891957145 cites W2006425381 @default.
• W2891957145 cites W2019310190 @default.
• W2891957145 cites W2022951808 @default.
• W2891957145 cites W2027761488 @default.
• W2891957145 cites W2029712803 @default.
• W2891957145 cites W2049628073 @default.
• W2891957145 cites W2056584048 @default.
• W2891957145 cites W2059982813 @default.
• W2891957145 cites W2062109850 @default.
• W2891957145 cites W2063546675 @default.
• W2891957145 cites W2065185272 @default.
• W2891957145 cites W2070095213 @default.
• W2891957145 cites W2079923248 @default.
• W2891957145 cites W2081166419 @default.
• W2891957145 cites W2085660362 @default.
• W2891957145 cites W2088209646 @default.
• W2891957145 cites W2088213501 @default.
• W2891957145 cites W2095297988 @default.
• W2891957145 cites W2100853152 @default.
• W2891957145 cites W2114402972 @default.
• W2891957145 cites W2114434420 @default.
• W2891957145 cites W2122437722 @default.
• W2891957145 cites W2124466530 @default.
• W2891957145 cites W2127051919 @default.
• W2891957145 cites W2132826741 @default.
• W2891957145 cites W2135257207 @default.
• W2891957145 cites W2137557732 @default.
• W2891957145 cites W2144925336 @default.
• W2891957145 cites W2153114310 @default.
• W2891957145 cites W2154845609 @default.
• W2891957145 cites W2155409809 @default.
• W2891957145 cites W2463691290 @default.
• W2891957145 cites W2517344722 @default.
• W2891957145 cites W2592400523 @default.
• W2891957145 cites W2598090898 @default.
• W2891957145 cites W2772373245 @default.
• W2891957145 cites W3109651676 @default.
• W2891957145 cites W48015990 @default.
• W2891957145 doi "https://doi.org/10.1130/b31722.1" @default.
• W2891957145 hasPublicationYear "2018" @default.
• W2891957145 type Work @default.
• W2891957145 sameAs 2891957145 @default.
• W2891957145 citedByCount "7" @default.
• W2891957145 countsByYear W28919571452020 @default.
• W2891957145 countsByYear W28919571452021 @default.
• W2891957145 countsByYear W28919571452022 @default.
• W2891957145 countsByYear W28919571452023 @default.
• W2891957145 crossrefType "journal-article" @default.
• W2891957145 hasAuthorship W2891957145A5000154624 @default.
• W2891957145 hasAuthorship W2891957145A5009827828 @default.
• W2891957145 hasAuthorship W2891957145A5012112613 @default.
• W2891957145 hasAuthorship W2891957145A5021142496 @default.
• W2891957145 hasAuthorship W2891957145A5061081115 @default.
• W2891957145 hasAuthorship W2891957145A5068880809 @default.
• W2891957145 hasAuthorship W2891957145A5076447304 @default.
• W2891957145 hasConcept C109007969 @default.
• W2891957145 hasConcept C114793014 @default.
• W2891957145 hasConcept C127313418 @default.
• W2891957145 hasConcept C142362112 @default.
• W2891957145 hasConcept C15708023 @default.
• W2891957145 hasConcept C166957645 @default.
• W2891957145 hasConcept C205649164 @default.
• W2891957145 hasConceptScore W2891957145C109007969 @default.
• W2891957145 hasConceptScore W2891957145C114793014 @default.
• W2891957145 hasConceptScore W2891957145C127313418 @default.
• W2891957145 hasConceptScore W2891957145C142362112 @default.
• W2891957145 hasConceptScore W2891957145C15708023 @default.
• W2891957145 hasConceptScore W2891957145C166957645 @default.
• W2891957145 hasConceptScore W2891957145C205649164 @default.

• next