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Parrilla

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Journal Article
Published: 01 February 1988
Journal of the Geological Society (1988) 145 (1): 147–155.
...J. Mangas; A. Arribas Abstract The Parrilla orebody, located on the southern border of the Cáceres province, is a stockwork of quartz veins with scheelite and cassiterite. The Sn-W ore fills fractures in the Greywacke Schist Complex, intruded in this area by Hercynian granites. Most of the veins...
Journal Article
Published: 01 June 2016
Journal of Sedimentary Research (2016) 86 (6): 637–667.
... zooxanthellate coral communities to constrain and model paleo-salinities of marginal-marine waters of the Miocene Lorca Basin, Spain. Salinities ranged from 22 to 32 PSU during growth of coral bioherms and carpets of the Soriana and Parrilla formations, and from 35 to 39 PSU during deposition of the Hondo...
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Book Chapter

Author(s)
E. Dapena, A. Parrilla
Series: Geological Society, London, Engineering Geology Special Publications
Published: 01 January 2012
DOI: 10.1144/EGSP26.7
EISBN: 9781862396333
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The Las Canteras locality (see Fig. 1). For explanation of units x1, 1a, 1b, and 1c, see Figure 2. L1–L6, logged sections through the Soriana and Parrilla formations. Position of oyster samples is shown for each log.
Published: 01 June 2016
Fig. 3.— The Las Canteras locality (see Fig. 1 ). For explanation of units x1, 1a, 1b, and 1c, see Figure 2 . L1–L6, logged sections through the Soriana and Parrilla formations. Position of oyster samples is shown for each log.
Journal Article
Journal: Economic Geology
Published: 01 December 1988
Economic Geology (1988) 83 (8): 1975–1984.
...Tawn Albinson Fatiguant; Luis Victor Parrilla Pineda GeoRef, Copyright 2004, American Geological Institute. 1988 ...
Image
Published: 01 June 2016
x1, 1a, etc. within the Soriana, Parrilla,and Hondo formations are informal stratigraphic units ( Thrana 2006 ). nd = not determined .
Image
A) δ18O vs. 87Sr/86Sr for the nondiagenetic oyster samples. Note the inferred non-oceanic samples (see text). B) Numerical age estimation based on inferred oceanic 87Sr/86SrMEAN values (Table 7). These data suggest a Tortonian age for the Soriana and Parrilla formations, and a Messinian age for the Hondo Formation (see text). The global Sr curve is from McArthur et al. (2001).
Published: 01 June 2016
Fig. 15.— A) δ 18 O vs. 87 Sr/ 86 Sr for the nondiagenetic oyster samples. Note the inferred non-oceanic samples (see text). B) Numerical age estimation based on inferred oceanic 87 Sr/ 86 Sr MEAN values ( Table 7 ). These data suggest a Tortonian age for the Soriana and Parrilla
Image
Location maps, geology, and stereographic projections of poles to veins in the studied areas. A. Cligga Head, Corn-wall, U.K. (after Moore and Jackson, 1977). B. St. Michael′s Mount, Cornwall, U.K. (after Hall, 1971). C. La Parrilla mine, Cáceres, Spain (after Gumiel and Pineda, 1981). D. Arroyomolinos, Cáceres, Spain (after Gumiel and Campos, 1998). E. Barruecopardo, Salamanca, Spain (after Arribas, 1979).
Published: 01 August 2008
F ig . 1. Location maps, geology, and stereographic projections of poles to veins in the studied areas. A. Cligga Head, Corn-wall, U.K. (after Moore and Jackson, 1977 ). B. St. Michael′s Mount, Cornwall, U.K. (after Hall, 1971 ). C. La Parrilla mine, Cáceres, Spain (after Gumiel and Pineda
Image
Log-log plots of cumulative number of veins (N) versus vein thickness (t). A. Data from Cligga Head showing significantly different distributions, with the mineralized site (Cligga 2) having a much lower scaling exponent (slope) that the unmineralized site (Cligga 1). B. Plots from the Caceres area (after Roberts et al., 1998) with mineralized site (La Parrilla) having much lower scaling exponent than at unmineralized site (Trujillo).
Published: 01 August 2008
the Caceres area (after Roberts et al., 1998 ) with mineralized site (La Parrilla) having much lower scaling exponent than at unmineralized site (Trujillo).
Image
Log-log plots of cumulative number of veins (N) versus vein thickness (t). A. Data from Cligga Head showing significantly different distributions, with the mineralized site (Cligga 2) having a much lower scaling exponent (slope) that the unmineralized site (Cligga 1). B. Plots from the Caceres area (after Roberts et al., 1998) with mineralized site (La Parrilla) having much lower scaling exponent than at unmineralized site (Trujillo).
Published: 01 August 2008
the Caceres area (after Roberts et al., 1998 ) with mineralized site (La Parrilla) having much lower scaling exponent than at unmineralized site (Trujillo).
Journal Article
Journal: Economic Geology
Published: 01 August 2008
Economic Geology (2008) 103 (5): 1043–1056.
...F ig . 1. Location maps, geology, and stereographic projections of poles to veins in the studied areas. A. Cligga Head, Corn-wall, U.K. (after Moore and Jackson, 1977 ). B. St. Michael′s Mount, Cornwall, U.K. (after Hall, 1971 ). C. La Parrilla mine, Cáceres, Spain (after Gumiel and Pineda...
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Geological map and stratigraphic column of the southern Lorca Basin as suggested by previous authors (Geel 1976; Wrobel 1999; Wrobel and Michalzik 1999; Thrana and Talbot 2006). Outcrops were studied at (1) Diecisiete Arcos and (2) Las Canteras. Figures modified from Vennin et al. (2004), and Thrana and Talbot (2006). Red lines are the Tortonian–Messinian boundary suggested by this study. The ? mark and vertical arrow indicate that the position of the Messinian–Tortonian boundary is uncertain (see text). The boundary between the Soriana and Parrilla formations is characterized by an angular unconformity (Thrana and Talbot 2006; Thrana 2006).
Published: 01 June 2016
al. (2004) , and Thrana and Talbot (2006) . Red lines are the Tortonian–Messinian boundary suggested by this study. The ? mark and vertical arrow indicate that the position of the Messinian–Tortonian boundary is uncertain (see text). The boundary between the Soriana and Parrilla formations
Image
The Diecisiete Arcos locality (see Fig. 1). Unit x1 is composed of marls pertaining to the Soriana Fm.; units 1a, 1b, and 1c are prograding carbonate-ramp deposits. Unit 2 is composed of mixed carbonates and siliciclastics (2a, predominantly beach gravels and alluvial-fan deposits and 2b, predominantly carbonate-ramp deposits). Unit 3 is composed of beach gravels and alluvial-fan deposits and unit 4 is a reef-rimmed carbonate platform (for further details on the sedimentology and sequence stratigraphy, see Thrana and Talbot 2006 and Thrana 2006). L7–L13, logged sections through the Soriana, Parrilla, and Hondo formations. Position of oyster samples are shown for each log.
Published: 01 June 2016
the Soriana, Parrilla, and Hondo formations. Position of oyster samples are shown for each log.
Journal Article
Published: 01 February 2008
The Canadian Mineralogist (2008) 46 (1): 87–109.
... one of the most representative and best studied deposits is La Parrilla, located about 90 km south of Los Santos, but formed in an equivalent setting within the lowermost Complejo Esquisto Grauváquico ( Gumiel & Pineda 1981 , Mangas & Arribas 1988 ). Here, NE-trending veins bearing scheelite...
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Journal Article
Journal: Economic Geology
Published: 01 August 2003
Economic Geology (2003) 98 (5): 1029–1037.
...) , Taylor (1971) , in Randall et al. (1994) Real de Guadalupe Guerrero 37–40 K-Ar 1 Albinson and Parrilla (1988) Taxco Guerrero 38–36? K-Ar 1 Alaniz-Álvarez et al. (2002) 2 Pachuca-Real del Monte Hidalgo 20.3 K-Ar McKee et al. (1992) Bolaños Jalisco 22.2...
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Journal Article
Published: 01 April 2016
Vadose Zone Journal (2016) 15 (4): vzj2015.01.0001rev.
... State Univ., Stillwater Paz-Ferreiro, J., Madrid, Spain Pedrera Parrilla, A., IFAPA, Sevilla, Spain Perfect, E., Univ. of Tennessee, Knoxville Persson, M., Lund Univ., Sweden Peth, S., Univ. of Kassel, Witzenhausen, Germany Plauborg, F., Aarhus Univ., Tjele, Denmark Qu, W...
Journal Article
Published: 01 October 2015
Journal of Foraminiferal Research (2015) 45 (4): 344–353.
... ). The latter two are separated by a large NE-SW trending antiform, the Alboran Ridge ( Comas et al., 1999 ). Modern oceanographic conditions in the Alboran Sea have been extensively described by La Violette (1984) , Parrilla et al. (1986) , Heburn & La Violette (1990) , and Rohling et al. (1995...
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Journal Article
Journal: Geophysics
Published: 08 August 2022
Geophysics (2022) 87 (5): E335–E346.
... ; Rejiba et al., 2018 ), archaeological prospection (e.g.,  Bongiovanni et al., 2008 ; De Smedt et al., 2011 ), and agricultural application (e.g.,  Pedrera-Parrilla et al., 2016 ; Badewa et al., 2018 ). Due to the indirect and band-limited nature of the FDEM data, predicting the spatial distribution...
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Journal Article
Journal: Geophysics
Published: 19 December 2024
Geophysics (2025) 90 (1): E13–E27.
... and processes of interest in various application domains, such as agriculture (e.g.,  Pedrera-Parrilla et al., 2016 ; von Hebel et al., 2021 ), landscape archaeology (e.g.,  De Smedt et al., 2013 ), and environmental assessment (e.g.,  Van De Vijver et al., 2015 ). Multireceiver FDEM data, considering...
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Journal Article
Published: 01 April 2010
The Canadian Mineralogist (2010) 48 (2): 375–390.
... & Arribas 1987 ), the Santa Comba mine ( Werner et al. 1998 ) and the Beariz district ( Gloaguen 2006 ) in the north, Golpejas ( Mangas 1981 , Arribas et al. 1981 ) and the Fregeneda pegmatites ( Roda Robles 1993 ) in the central part, and La Parrilla ( Gumiel & Pineda 1981 ) and Teba ( Mangas...
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