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Los Lobos Field

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Journal Article
Journal: AAPG Bulletin
Published: 01 August 1994
AAPG Bulletin (1994) 78 (8): 1257–1275.
... in the local fold axes and reverse faults of Pliocene age and younger. Second, at the extreme southern reaches of the SSJV in the San Emidio, Los Lobos, Pleito, Wheeler Ridge, and North Tejon fields, another systematic, but localized, reorientation in the stress field indicates an abrupt change...
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Map showing characteristics of San Ardo oil field and section numbers. Contoured surface is the top of the Lombardi sand (interval is 50 ft [15m]). Dots show locations of wells at surface. Purple dashed line shows limit of Lombardi reservoir production; green stippled line shows limit of Aurignac reservoir production. North Lombardi Fault, shown at reservoir depth, and surface trace of Los Lobos Fault are indicated. North Lombardi Fault is hachured to show downthrown side; barbs show overriding side of Los Lobos Fault.
Published: 01 December 2017
of Aurignac reservoir production. North Lombardi Fault, shown at reservoir depth, and surface trace of Los Lobos Fault are indicated. North Lombardi Fault is hachured to show downthrown side; barbs show overriding side of Los Lobos Fault.
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Location map for Salinas Basin, central California. A heavy outline delineates the basin boundary. East of the Rinconada Fault (RF), the boundary is a depositional limit, which lies in the subsurface; west of the fault, it is the erosional truncation in the outcrop of basin strata. Transect AA′ is the location of the cross section shown in Figure 2 and transects CC′ and DD′ are seismic reflection profiles in Figure 10. Shaded polygons refer to oil fields; abbreviations are the oil field names listed in the inset. Inset: size distribution of Salinas Basin oil fields. Recoverable oil estimates from California Division of Oil, Gas, and Geothermal Resources (2010). AST = Arroyo Seco trough; HVT = Hames Valley trough; LLF = Los Lobos Fault.
Published: 15 June 2019
oil estimates from California Division of Oil, Gas, and Geothermal Resources (2010) . AST = Arroyo Seco trough; HVT = Hames Valley trough; LLF = Los Lobos Fault.
Image
—Stress map of the southern San Joaquin Valley in the vicinity of the White Wolf fault. The inward facing arrows indicate the directions of the maximum horizontal principal compressive stress (SHmax) inferred from well-bore breakouts. Labeled stress symbols identify those data analyzed in this study. Shown are results from the Elk Hills, Mountain View, Paloma, Yowlumne North, Yowlumne, Rio Viejo, San Emidio, Pleito, Wheeler Ridge, North Tejon, and Los Lobos production fields. Data from each of the wells are represented in detail in Tables 1 and 2. The dashed lines are the fold axes (Page, 1981), which subparallel the shallow thrust faults (saw-toothed lines). The star is the epicentral location of the 1952 Ms 7.8 Kern County earthquake. Cross section AA’ is shown in Figure 13.
Published: 01 August 1994
in this study. Shown are results from the Elk Hills, Mountain View, Paloma, Yowlumne North, Yowlumne, Rio Viejo, San Emidio, Pleito, Wheeler Ridge, North Tejon, and Los Lobos production fields. Data from each of the wells are represented in detail in Tables 1 and 2 . The dashed lines are the fold axes ( Page
Journal Article
Journal: GSA Bulletin
Published: 01 January 2000
GSA Bulletin (2000) 112 (1): 86–97.
... Wolf fault, the Pleito and Wheeler Ridge faults of the Pleito fault system, and the newly identified Los Lobos fault. These faults form the northern boundary of the San Emigdio Mountain front. The dominant structural features of the north flank of the San Emigdio Mountains are east-west–trending folds...
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(A) Diagram shows 3He/4He vs. 4He/20Ne (after Sano and Wakita, 1985) for dissolved and free gas samples from Celaya (Cel)–Querétaro (Qro)–San Juan del Río (SJR) aquifers and Los Azufres geothermal field. Air (air) and ASW (air-saturated water) denote the atmospheric end-members (the first for the free gas and the second for the dissolved gas). The solid lines show the mixture of the atmospheric end-members with mantle end-members. The 4He/20Ne end-member ratios used are 0.265 for air and ASW (Smith and Kennedy, 1983) and 1000 for crustal and mantellic fluids (Sano and Wakita, 1985). The R/Ra end-member ratios used are 1 Ra for Air, 0.983 Ra for ASW (Benson and Krause, 1980), 0.02 Ra for the crust (Hooker et al., 1985), and 7.3 Ra for the lithospheric mantle in Mexico (Straub et al., 2011). Data from Los Azufres were taken from Pinti et al. (2013) and Wen et al. (2018). Data from El Geyser were taken from González-Guzmán et al. (2019). HTGW—high-temperature groundwater; LTGW—low-temperature groundwater. No error bars are shown because they are similar to or smaller than the symbol size. Solid gray and black lines are the mixing curves between the air and mantle and the ASW and mantle end-members, respectively. (B) Atmosphere–crust–mantle ternary diagram. Santa Cruz Forajes (SCF), Saldarraga (Sal), El Lobo (EL), La D (LD), Palmillas (Pal), Amealco (Ame), and Celaya Geothermal Well (PC) are sample names.
Published: 12 December 2022
Figure 5. (A) Diagram shows 3 He/ 4 He vs. 4 He/ 20 Ne (after Sano and Wakita, 1985 ) for dissolved and free gas samples from Celaya (Cel)–Querétaro (Qro)–San Juan del Río (SJR) aquifers and Los Azufres geothermal field. Air (air) and ASW (air-saturated water) denote the atmospheric end
Journal Article
Journal: AAPG Bulletin
Published: 15 June 2019
AAPG Bulletin (2019) 103 (6): 1443–1472.
... oil estimates from California Division of Oil, Gas, and Geothermal Resources (2010) . AST = Arroyo Seco trough; HVT = Hames Valley trough; LLF = Los Lobos Fault. ...
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Journal Article
Journal: The Leading Edge
Published: 01 July 2001
The Leading Edge (2001) 20 (7): 763–782.
... of the Golden Lane offshore Mexico play. The marine extension of the Golden Lane was delineated with analog seismic surveys in 1957. Six years later, in 1963, the first field in the offshore structure, Isla de Lobos, was discovered. Well Isla de Lobos-1B found oil in the El Abra Formation 2096 m...
FIGURES | View All (6)
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1936
AAPG Bulletin (1936) 20 (4): 467–477.
...SAN ANTONIO GEOLOGICAL SOCIETY 1 This log and accompanying map were used on the 6th annual field trip of the San Antonio Geological Society, November 4 and 5, 1934. Subsequent changes in the road have probably changed slightly the mileage shown in this log. 2 Officers in 1934...
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Journal Article
Journal: AAPG Bulletin
Published: 01 September 1980
AAPG Bulletin (1980) 64 (9): 1476–1483.
... Olmos production with the 1 Stumberg Ranch ( Table 2 , no. 3), the discovery well for Stumberg field. Petrorock, Inc., found pay in the San Miguel Formation with the 1 Wilson-Risinger ( Table 2 , no. 4). This find was designated as the Petro-Rock field. In Maverick County, the Los Quatros North...
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Journal Article
Published: 01 April 2011
Earth Sciences History (2011) 30 (1): 135–163.
... to be published in O Instituto . These observations were initiated in the early nineteenth century. In 1812, Constantino Botelho de Lacerda Lobo (1754–1820), Professor of Physics at the Philosophy Faculty of the UC, published meteorological observations in the Jornal de Coimbra from January 1812 to March 1817...
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Journal Article
Journal: AAPG Bulletin
Published: 01 October 1989
AAPG Bulletin (1989) 73 (10B): 141–146.
... listed in Table 6 . Inset map shows Texas Railroad Commission (RRC) districts. Figure 2 —Structure map on top of middle House 8 sand, Bonne Terre field, McMullen County, Texas. Note Argo 1 Tucker et al well, which produced from same closure at top of upper Wilcox. Lobo Resources...
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Journal Article
Journal: AAPG Bulletin
Published: 01 December 2017
AAPG Bulletin (2017) 101 (12): 1917–1943.
... of Aurignac reservoir production. North Lombardi Fault, shown at reservoir depth, and surface trace of Los Lobos Fault are indicated. North Lombardi Fault is hachured to show downthrown side; barbs show overriding side of Los Lobos Fault. ...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1962
AAPG Bulletin (1962) 46 (11): 2090–2098.
... Group and Fusselman Formation, Franklin Mountains, Texas : West Tex. Geol. Soc. Guidebook, 1958 Field Trip , p. 30 – 42 . Yochelson , E. L. , 1956 , Permian Gastropoda of the southwestern United States : Am. Mus. Nat. History Bull. , v. 110 , art. 3, p. 179 – 275 . Zeller , R...
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Journal Article
Published: 27 May 2022
Geological Magazine (2022) 159 (8): 1454–1470.
... highlights the importance of palynostratigraphy and detrital zircon geochronology for an integrated understanding of the depositional age and paleoenvironmental models, confirming the field-based interpretations of the complex stratigraphy of the southern sector of the Pulo do Lobo Domain...
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Journal Article
Journal: Elements
Published: 01 October 2016
Elements (2016) 12 (5): 341–346.
... source of the coin metal is the valley of Los Pedroches (Andalusia, southern Spain), which was well known at the time for its Ag, Cu, Pb and Zn ores, and has a Pb isotopic composition that falls within the field of Group 1 coins. Most of the 92 naturally occurring elements have been used to compare...
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Journal Article
Journal: AAPG Bulletin
Published: 01 August 1978
AAPG Bulletin (1978) 62 (8): 1511–1518.
... corp. has completed a significant discovery in the Rodessa Formation. The 1 Burr Ranch ( Table 2 , no. 11) flowed at the rate of 33 MMCFGD with an AOF of 237 MMCFGD. The discovery will be designated the Los Quatros field. Also in Edwards County, Sun Oil Co. has completed the 1 C.D. Hopkins ( Table 2...
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Journal Article
Published: 01 May 2025
Earthquake Spectra (2025) 41 (2): 1536–1564.
... and Environmental Engineering, Universidad de los Andes, Carrera 1 Este No. 19A - 40, Edificio Mario Laserna, Bogotá 11171, Colombia. Email: [email protected] 8 10 2024 4 1 2025 © The Author(s) 2025 2025 Earthquake Engineering Research Institute Unreinforced masonry unreinforced...
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Journal Article
Published: 20 December 2022
Journal of Sedimentary Research (2022) 92 (12): 1116–1140.
...Álvaro Carrión-Torrente; Francisco José Lobo; Ángel Puga-Bernabéu; Isabel Mendes; Susana Lebreiro; Marga García; David van Rooij; María Luján; María Isabel Reguera; Laura Antón Abstract The postglacial sea-level rise after the Last Glacial Maximum provided ideal conditions to study...
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Journal Article
Published: 01 November 2006
Earthquake Spectra (2006) 22 (4): 1035–1061.
... of 1 m.s −1 and 2 m.s −1 occur in the Los Angeles Basin and San Fernando Valley, respectively, while the corresponding peak displacements are about 1 m and 2 m , respectively. Peak interstory drifts in the two buildings exceed 0.10 and 0.06 in many areas of the San Fernando Valley and the Los Angeles...