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Cuzco fault system

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Journal Article
Published: 01 February 1998
Bulletin of the Seismological Society of America (1998) 88 (1): 242–255.
...Justo Cabrera; Michel Sébrier Abstract The shallow, mb = 5.3, 1986 earthquake that affected the Cuzco region reactivated the 18-km-long Chincheros-Qoricocha faults in the central part of the Cuzco fault system. Although the event has a moderate magnitude, clear surface ruptures were observed...
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Field view of the Tambomachay <span class="search-highlight">fault</span>, a member of the <span class="search-highlight">Cuzco</span>-Vilcanota <span class="search-highlight">fault</span> ...
Published: 01 November 2015
Figure 2. Field view of the Tambomachay fault, a member of the Cuzco-Vilcanota fault system, seen toward the west from near point O on Figure 1 . Field of view along range front is ∼5 km wide. Inset shows location of Cuzco-Vilcanota fault system (CVFS) relative to exposures of Rumicolca back-arc
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(A) Sr and Nd isotopic compositions for group 1 and group 2 Peruvian xenoli...
Published: 01 November 2015
Figure 9. (A) Sr and Nd isotopic compositions for group 1 and group 2 Peruvian xenoliths compared to Bolivian xenoliths ( McLeod et al., 2013 ), back-arc lavas ( Chapman and Ducea, 2013 ), and Paleozoic basement rocks ( Lucassen et al., 2001 ) exposed along the Cuzco-Vilcanota fault system (CVFS
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F ig . 6. Schematic paleogeographic reconstruction of the study area during...
Published: 01 December 2003
. Also shown are the main fault systems and high-angle thrusts that are interpreted to have controlled both uplift of the batholith at the deformation front south of Cuzco (the Cuzco-Puno high) and the San Jerónimo basins. Main localities are shown for reference. Modified after Carlotto (1998) .
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Geologic map modified after   Mapa Geológico del Perú  (1975)  showing loca...
Published: 01 November 2015
Figure 1. Geologic map modified after Mapa Geológico del Perú (1975) showing locations of Rumicolca (black stars) and Puno suite (white stars) exposures, and sampled xenolith localities (H—Huarocondo; N—Tipon; O—Oropesa; P—Puno; R—Raqchi; Y—Taray). Cuzco-Vilcanota fault system runs from Cuzco
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(A) Major-element variation diagrams for Peruvian xenoliths compared to bac...
Published: 01 November 2015
Figure 8. (A) Major-element variation diagrams for Peruvian xenoliths compared to back-arc lavas ( Chapman and Ducea, 2013 ) exposed along the Cuzco-Vilcanota fault system (CVFS). FeO* denotes total Fe as FeO. (B) Normal mid-ocean-ridge basalt (N-MORB)–normalized trace-element and chondrite
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(A) Major-element variation diagrams for Peruvian xenoliths compared to bac...
Published: 01 November 2015
Figure 8. (A) Major-element variation diagrams for Peruvian xenoliths compared to back-arc lavas ( Chapman and Ducea, 2013 ) exposed along the Cuzco-Vilcanota fault system (CVFS). FeO* denotes total Fe as FeO. (B) Normal mid-ocean-ridge basalt (N-MORB)–normalized trace-element and chondrite
Journal Article
Journal: GSA Bulletin
Published: 01 November 2015
GSA Bulletin (2015) 127 (11-12): 1777–1797.
...Figure 2. Field view of the Tambomachay fault, a member of the Cuzco-Vilcanota fault system, seen toward the west from near point O on Figure 1 . Field of view along range front is ∼5 km wide. Inset shows location of Cuzco-Vilcanota fault system (CVFS) relative to exposures of Rumicolca back-arc...
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Journal Article
Journal: Economic Geology
Published: 01 December 2003
Economic Geology (2003) 98 (8): 1575–1605.
.... Also shown are the main fault systems and high-angle thrusts that are interpreted to have controlled both uplift of the batholith at the deformation front south of Cuzco (the Cuzco-Puno high) and the San Jerónimo basins. Main localities are shown for reference. Modified after Carlotto (1998) . ...
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Series: Geological Society, London, Special Publications
Published: 01 January 2009
DOI: 10.1144/SP310.3
EISBN: 9781862395589
... for llamas and alpacas. It has been proved that the layout of some cities was based on hydrological criteria. The most obvious case is Cuzco, where administrative districts were organized, inside the metropolitan area, based on irrigation systems ( Sherbondy 1987 ); that is, first the channels...
FIGURES
Journal Article
Journal: Economic Geology
Published: 01 March 2009
Economic Geology (2009) 104 (2): 267–289.
.... The mineralized zone (indicated resources 5.1 Mt @ 8.2% Zn and 0.9% Pb) occupies the hinge of an anticlinal dome that has been exposed by erosion. The southern limb of the structure dips about 55° to the south-southwest, whereas its northern limb is truncated by faults. The nonsulfide concentrations, consisting...
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Journal Article
Published: 01 September 2001
Geological Magazine (2001) 138 (5): 628–629.
... to be considered always within the historical context. Hancock et al. focus on the Roman city of Heirapolis, Turkey, and discuss interrelationships between earthquake faulting, travertine deposition, and seismicity. They consider the exploitation of the travertine for building stone in the city, and how...
Journal Article
Journal: GSA Bulletin
Published: 01 September 2009
GSA Bulletin (2009) 121 (9-10): 1298–1324.
... one remnant of a Late Ordovician intrusive belt is recognized in the Cuzco batholith (446.5 ± 9.7 Ma) indicating that the Famatinian arc system previously identified in Peru along the north-central Eastern Cordillera and the coastal Arequipa-Antofalla terrane also existed inboard...
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Journal Article
Published: 01 August 2001
Bulletin of the Seismological Society of America (2001) 91 (4): 694–707.
... part of the Cuzco fault system, characterized by a normal fault mechanism ( Cabrera and Sébrier, 1998 ), a clear instance of surface rupture was observed totaling 3 km in length, with a maximum normal displacement of 10 cm. Events of this type are governed by their own scaling law, differing from...
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Journal Article
Published: 23 November 2020
Journal of the Geological Society (2021) 178 (2): jgs2020-100.
... on the Permo-Triassic granitic Machu Picchu Batholith (Eastern Cordillera; Fig. 1 ), emplaced at 222 ± 7 Ma ( Carlier et al. 1982 ). The regional crustal-scale Apurimac fault system, c . 15 km south of the Machu Picchu Batholith, delimits two lithospheric blocks ( Carlier et al. 2005 ) corresponding...
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Journal Article
Published: 01 October 1962
Bulletin of the Seismological Society of America (1962) 52 (4): 793–805.
... . (in preparation) Bulletin of the Seismological Society of America. Vol. 52, No. 4, pp. 793-805. October, 1962 THE SAN AGUSTIN FAULT SYSTEM OF SOUTHERN PERU BY A. RODRIGUEZ B., J. S. STEINHART, AND T. ASADA ABSTRACT A study of the hypocentral location of 133small earthquakes in southern Peru reveals the exist...
Journal Article
Published: 27 September 2016
Bulletin of the Seismological Society of America (2016) 106 (6): 2532–2544.
... by different authors. Initials for every fault trace in Figure  1 refer to the name of the fault systems described below. Among the main fault systems in the basin are the La Pera fault system ( PE ) ( Lermo et al. , 1995 ; Delgado‐Granados et al. , 1997 ; Ávila‐Bravo, 1998 ; De Cserna et al. , 1998...
Journal Article
Published: 01 December 1998
Bulletin of the Seismological Society of America (1998) 88 (6): 1589–1611.
... Cabrera, Justo and Michel Sebrier, Surface Rupture Associated with a 5.3-rob Earthquake: the 5 April 1986 Cuzco 1392 Earthquake and Kinematics of the Chincheros-Qoricocha Faults of the High Andes, Peru 1402 California, Comparison of Recent Probabilistic Seismic Hazard Maps for Southern, by Mark W...
Journal Article
Published: 25 April 2023
Seismological Research Letters (2023) 94 (4): 1775–1790.
... with coseismic surface faulting , Environ. Eng. Geosci. xxv , 17 – 29 , doi: 10.2113/gseegeosci.xxv.1.17 . Cabrera J. , and Sébrier M. 1998 . Surface rupture associated with a 5.3‐mb earthquake: The 5 April 1986 Cuzco earthquake and kinematics of the Chincheros‐Quoricocha faults of the High...
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Journal Article
Published: 12 July 2016
Bulletin of the Seismological Society of America (2016) 106 (4): 1423–1437.
... portion of the basin is delimited by the Chichinautzin range, the Nevada range, and the Las Cruces range. The main fault systems are identified by solid circles with two letters: La Pera (PE), Azteca (AZ), Xochimilco (XO), Xicomulco (XI), Sub‐cuenca de Chalco (CH), Mixhuca (MI), Contreras (CO), Ixtlahuaca...
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