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  • Mohorovicic discontinuity
    ...cally occurs approximately 35 km (~19 mi) below the continents and 5 to 10 km (3-5 mi) below the floor of the ocean.<ref name=Petersetal_2012>Peters, Ken
    729 bytes (103 words) - 15:49, 4 December 2015
  • User:Matt/- Sobrarbe Formation
    ...onian sediments in the Ainsa Basin<ref>Dreyer et al</ref>. It contains 5.5 km of continuous outcrop exposure from the shelf-edge delta to the distal slop ...he south of the town of Ainsa, Huesca, Spain. It is about 25 km wide by 75 km long, and is bound on the east by the Rio Cinca, and the west by the Colina
    1 KB (163 words) - 00:12, 30 June 2014
  • File:BlackWarriorBasinFG1.JPG
    Black Warrior Basin. 20 mi (32 km). From Fritz et al., 2012, Great American Carbonate Bank: Knox Group in the
    (800 × 563 (178 KB)) - 15:47, 5 January 2015
  • File:M91FG196.JPG
    Ooid shoal, Bahamas; the bottom edge of the photograph represents a 4.5-km (2.7 mi)-wide transect. The lower inset is an illustration of a cliff expos
    (800 × 909 (88 KB)) - 13:08, 20 August 2015
  • File:M106Ch07Fig07.jpg
    ...w of hydrocarbon shows in Jordanian petroleum wells. After NRA (2001). 100 km (62.1 mi). From Luning, S., and J. Kuss, 2014, Petroleum geology of Jordan,
    (700 × 735 (86 KB)) - 21:41, 18 April 2016
  • File:M106Ch04Fig03.jpg
    Sedimentary basins of Libya (productive basins, future prospective) 200 km (124.3 mi). From Hassan, H. S., and C. C. G. Kendall, 2014, Hydrocarbon pro
    (700 × 676 (77 KB)) - 20:13, 28 March 2016
  • File:M91FG181.JPG
    ...llite photo of a braided river in Tibet. The braided river belt is about 7 km (4 mi) wide. Courtesy of the NASA Web site (www.earthobservatory.nasa.gov).
    (600 × 805 (104 KB)) - 21:18, 10 August 2015
  • File:M106Ch07Fig1.jpg
    ...fields in Jordan. Modified after Beydoun et al. (1994) and NRA (2001). 100 km (62.1 mi). From Luning, S., and J. Kuss, 2014, Petroleum geology of Jordan,
    (700 × 857 (97 KB)) - 20:28, 18 April 2016
  • File:M91Ch11FG69.JPG
    ...ial fan in China's Xinjuang Province. The diameter of the fan is about 170 km (106 mi). Courtesy of the NASA Web site: www.earthasart.gsfc.nasa.gov. Show
    (600 × 606 (106 KB)) - 15:42, 27 April 2015
  • File:M106Ch13Fig11.jpg
    ...Adana and İskenderun subbasins (redrawn from Derman and Gürbüz, 2007). 10 km (6.2 mi). From Derman, Ahmet Sami, 2014, Petroleum systems of Turkish Basin
    (700 × 637 (109 KB)) - 20:03, 5 July 2016
  • File:M106Ch12Fig06.jpg
    ...cross the Mesopotamian Foredeep to the Zagros foldbelt in eastern Iraq. 50 km (31.1 mi). From Grabowski Jr., G. J., 2014, Iraq, in L. Marlow, C. Kendall,
    (690 × 337 (55 KB)) - 13:59, 12 May 2016
  • File:M106h04Fig01.jpg
    ...ajor tectonic elements (modified after Rusk, 2001; Ramos et al., 2006) 500 km (310.7 mi). From Hassan, Hassan S. and Christopher C. G. Kendall, Hydrocarb
    (700 × 439 (50 KB)) - 19:01, 28 March 2016
  • File:M106Ch07Fig05.jpg
    ...orthern Arabia and Northeast Africa. After Stampfli and Borel (2002). 1500 km (932 mi). From Lüning et al. (2006). From Luning, S., and J. Kuss, 2014, P
    (700 × 468 (49 KB)) - 21:06, 18 April 2016
  • File:M115CH10FG03.jpg
    ...gh the Miller field area to the distal margin near the Kingfisher field 15 km (9 mi) to the northeast. Modified after [[Kingfisher field|Turner et al. (1
    (1,076 × 597 (435 KB)) - 18:42, 17 January 2019
  • File:M91FG186.JPG
    ...asart.gsfc.nasa.gov). The inset box on the photograph measures 34 times 42 km (21 times 26 mi). The lower diagram is a box diagram showing the sedimentol
    (800 × 1,137 (157 KB)) - 19:22, 13 August 2015
  • File:M91FG184.JPG
    ...f the NASA Web site (www.earthasart.gsfc.nasa.gov). The delta is about 200 km (124 mi) across in this view. The photograph has been rotated such that nor
    (800 × 1,134 (191 KB)) - 20:10, 12 August 2015
  • File:M106Ch14Fig01.jpg
    ...gure 2. Permian outcrops surrounding the Arabian shield are indicated. 200 km (124.3 mi). From M. L. Bordenave, 2014, Petroleum Systems and Distribution
    (641 × 662 (94 KB)) - 18:05, 12 July 2016
  • File:M106Ch14Fig12.jpg
    ...ndicating the regional highs as they appear before the Zagros folding. 100 km (62.1 mi). From M. L. Bordenave, 2014, Petroleum Systems and Distribution o
    (700 × 356 (74 KB)) - 19:40, 12 July 2016
  • File:M106Ch14Fig14.jpg
    ...al highs close to the Mesopotamian depression area are also indicated. 100 km (62.1 mi). From M. L. Bordenave, 2014, Petroleum Systems and Distribution o
    (700 × 402 (73 KB)) - 19:35, 12 July 2016
  • File:M106Ch06Fig03.jpg
    ...ormation in the Israel Ministry of Energy and Water Resources website). 50 km (31.1 mi). From Gardosh, Michael A., and Eli Tannenbaum, 2014, The petroleu
    (700 × 917 (76 KB)) - 15:29, 23 February 2016
  • File:M31F24.jpg
    ...ide gullies in the Mississippi River delta. The width of the mosaic is 1.5 km, and the superimposed grid is a 25-m square. The slope is from top (approxi
    (758 × 947 (524 KB)) - 18:21, 18 August 2014
  • File:M106Ch14Fig11.jpg
    ...al highs close to the Mesopotamian depression area are also indicated. 100 km (62.1 mi). From M. L. Bordenave, 2014, Petroleum Systems and Distribution o
    (700 × 422 (79 KB)) - 18:36, 12 July 2016
  • File:M106Ch04Fig2B.jpg
    ...s: Klitzsch (1971), Zegaar (1986), Anketell (1996), and Hallett (2002) 500 km (310.7 mi). From Hassan, H. S., and C. C. G. Kendall, 2014, Hydrocarbon pro
    (700 × 635 (73 KB)) - 19:43, 28 March 2016
  • File:M106Ch04Fig2A.jpg
    ...s: Klitzsch (1971), Zegaar (1986), Anketell (1996), and Hallett (2002) 500 km (310.7 mi). From Hassan, H. S., and C. C. G. Kendall, 2014, Hydrocarbon pro
    (700 × 633 (66 KB)) - 19:44, 28 March 2016
  • File:M106Ch07Fig04.jpg
    ...adjusted according to offset shale baseline. From Lüning et al. (2006). 5 km (3.1 mi). From Lüning et al. (2006). From Luning, S., and J. Kuss, 2014, P
    (564 × 855 (75 KB)) - 20:49, 18 April 2016
  • Sandbox
    We can also convert distances like [[distance::25 km]] and depths like [[depth::12000 ft]].
    571 bytes (74 words) - 18:30, 8 August 2013
  • File:M106Ch12Fig02.jpg
    ...to be caused by the structural grain of Precambrian accreted terrains. 200 km (124.3 mi). From Grabowski Jr., G. J., 2014, Iraq, in L. Marlow, C. Kendall
    (700 × 373 (52 KB)) - 20:26, 11 May 2016
  • File:M106Ch13Fig01.jpg
    ...y an ophiolitic suite of rocks (redrawn from Şengör and Yilmaz, 1981). 300 km (186.4 mi). From Derman, Ahmet Sami, 2014, Petroleum systems of Turkish Bas
    (700 × 513 (90 KB)) - 19:29, 5 July 2016
  • Mantle
    ...he base of the [[crust]] to the core-mantle boundary at approximately 2900 km (-1802 mi) in depth.<ref name=Petersetal_2012>Peters, Kenneth E., David J.
    898 bytes (129 words) - 13:23, 3 August 2016
  • File:Mth14ch04f01.jpg
    South Pass 62 field is located 50 km southeast of the mouth of the Mississippi River in 100 m of water. Dark gra
    (700 × 525 (111 KB)) - 16:00, 7 December 2015
  • Charge volume
    | 0 km<sup>2</sup> | 50 km<sup>2</sup>
    6 KB (834 words) - 20:41, 14 February 2022
  • File:M106Ch06Fig02.jpg
    ...Numbers refer to oil fields and hydrocarbon shows detailed in Table 1. 50 km (31.1 mi). From Gardosh, Michael A., and Eli Tannenbaum, 2014, The petroleu
    (489 × 824 (63 KB)) - 15:25, 23 February 2016
  • Magnetotellurics case history: frontier basin analysis (Amazon Basin, Colombia)
    ...ts, p. 428–499.</ref> This study area was very large approximately 300,000 km<sup>2</sup> (115,000 mi<sup>2</sup>) and remote with dense jungle cover, ru ...ompact. Data were collected from 43 sites, with a typical spacing of 10–20 km (6–12 mi).
    4 KB (480 words) - 15:12, 31 January 2022
  • File:M106Ch14Fig13.jpg
    ...abia), and migration paths from the kitchens toward the Gavbendi High. 100 km (62.1 mi). From M. L. Bordenave, 2014, Petroleum Systems and Distribution o
    (700 × 464 (101 KB)) - 18:44, 12 July 2016
  • Geothermal gradient
    ...ing fluids. Worldwide average geothermal gradients are from 24 to 41&deg;C/km (1.3-2.2&deg;F/100 ft), with extremes outside this range.<ref name=Peterset
    901 bytes (127 words) - 19:53, 25 June 2015
  • File:M114CH03FG03.jpg
    ...n the southern part of the basin are at burial depths present day of ca. 3 km and have not been significantly inverted. The large, deep fault northwest o
    (700 × 600 (112 KB)) - 17:49, 4 January 2019
  • Basement fault blocks and fault block patterns
    ...dicity to the shear zones, the spacing between them varying from about 4–8 km (2.5–5 mi). ...out [[length::1 km]] (LaBerge, personal communication) up to [[length::2.5 km]] or more.
    5 KB (617 words) - 19:55, 27 January 2022
  • Magnetics: interpreting residual maps
    ...n in a new basin, i.e., in determining whether it is 2, 5, or [[length::10 km]] thick, for example, to a usual accuracy of about ±15% under favorable co ...tion is approximately 3.6 km (12,000 ft) thick and basement lies about 3.8 km (12,500 ft) beneath flight level.]]
    8 KB (1,109 words) - 17:41, 24 January 2022
  • Kerogen type and maturity
    ...[vitrinite reflectance]], right figure) and follow across at [[length::2.1 km]] until you reach the maturity profile. This vitrinite reflectance value (0
    4 KB (503 words) - 14:18, 14 February 2022
  • 3-D seismic data: time and horizon slices
    ...this, at about the level indicated by the arrows, the section crosses a 1-km-wide Paleocene deep-water [[turbidite]] channel. ...tracted where the shifted surface intersects the 3-D volume of data. The 1-km-wide channel is unmistakable on this view of the data, and both edges of th
    4 KB (617 words) - 19:30, 27 January 2022
  • Black Warrior basin
    ...BasinFG1.JPG|thumb|300px|{{figure number|1}}Black Warrior Basin. 20 mi (32 km). From Fritz et al.<ref name=Fritzetal_2012>Fritz, R. D., P. Medlock, M. Ku
    2 KB (308 words) - 16:53, 26 March 2015
  • Braided fluvial reservoirs
    ...llite photo of a braided river in Tibet. The braided river belt is about 7 km (4 mi) wide. Courtesy of the [http://www.earthobservatory.nasa.gov NASA Web ...dimentary Research, v. 76, p. 731–770.</ref> quoted widths in excess of 40 km (25 mi) and thicknesses up to 1200 m (3937 ft) for the very large braided r
    13 KB (1,859 words) - 21:29, 12 March 2019
  • User:Matt
    * SMW quantities, e.g. [[distance::145 km]]
    2 KB (300 words) - 15:57, 8 April 2014
  • Plate tectonics and basin formation
    ===Major Plates (≥10 million km<sup>2</sup>)=== * Pacific Plate – 103,300,000 km<sup>2</sup>
    24 KB (3,689 words) - 17:46, 18 April 2019
  • Basin outline: Gulf of Mexico example
    ...arrows). It also shows the interpreted limits of thick Jurassic salt (>1.5 km). The geographic shifts of primary fluvial input have resulted in [[depocen
    3 KB (370 words) - 17:53, 18 February 2022
  • San Juan basin
    ...orner of New Mexico and in southern Colorado that encompasses about 35,000 km<sup>2</sup> (13,500 mi<sup>2</sup>). The [[basin]] contains deposits of [[n
    3 KB (411 words) - 15:01, 11 January 2016
  • Magnetotelluric survey case history: volcanic terrain (Columbia River Plateau)
    ...e Idaho-Washington border and extends approximately [[length::75 mi]] (120 km) to the west (Mills, personal communication, 1994).
    3 KB (359 words) - 15:15, 31 January 2022
  • Jordan petroleum geology
    ...es in Jordan: Directorate of petroleum exploration, Amman, 56 p.</ref> 100 km (62.1 mi). ...shale baseline. From L&uuml;ning et al.<ref name=L&uuml;ningetal_2006 /> 5 km (3.1 mi).]]
    16 KB (2,310 words) - 15:13, 19 January 2017
  • Surficial geochemical case history 3: Predrill–postdrill comparison
    ...ew hundred acres to regional programs covering 1,000 mi<sup>2</sup> (2,590 km<sup>2</sup>).
    4 KB (499 words) - 22:30, 31 January 2022
  • Electrical methods
    ...to investigating resistivities down to depths as great as 1 to [[length::2 km]], although greater depths of investigation are possible with some techniqu ...ounded wire systems are applicable to depths well in excess of [[length::1 km]], although high power transmitters are required as depth increases. The re
    15 KB (2,130 words) - 21:19, 19 January 2022

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