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Oceanus Anticline

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<span class="search-highlight">Oceanus</span> <span class="search-highlight">anticline</span> and fluid escape pipe trail. (A) Seismic profile (locatio...
Published: 12 January 2021
Figure 2. Oceanus anticline and fluid escape pipe trail. (A) Seismic profile (location in Fig. 1A ) through Oceanus and pipe trail. Numbered white arrows point to pockmarks at the outlet of each pipe, numbered 1–21 in order of formation. Synkinematic reflection geometry is present in the mid
Image
Pressure-depth ( P - z ) plots for pipe formation above <span class="search-highlight">Oceanus</span> <span class="search-highlight">anticline</span>. ...
Published: 12 January 2021
Figure 3. Pressure-depth ( P - z ) plots for pipe formation above Oceanus anticline. (A) P - z plot for last pipe (P21) in the trail, based on a reservoir filled with gas to its current trap capacity of 660 m; 81.2 MPa is pressure for pipe propagation across the top seal (intersection of gas
Image
Pressure evolution for early Miocene reservoir at the crest of <span class="search-highlight">Oceanus</span> anti...
Published: 12 January 2021
Figure 4. Pressure evolution for early Miocene reservoir at the crest of Oceanus anticline. (A) Gross pressure evolution from 5 Ma to present day, showing possible pressure buildup curve (solid blue line) with hypothetical upper and lower bounds (dotted lines) from the starting point
Journal Article
Journal: Geology
Published: 12 January 2021
Geology (2021) 49 (5): 576–580.
...Figure 2. Oceanus anticline and fluid escape pipe trail. (A) Seismic profile (location in Fig. 1A ) through Oceanus and pipe trail. Numbered white arrows point to pockmarks at the outlet of each pipe, numbered 1–21 in order of formation. Synkinematic reflection geometry is present in the mid...
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Image
Geological setting of the study area. (A) Bathymetric map (from GeoMapApp, ...
Published: 12 January 2021
Figure 1. Geological setting of the study area. (A) Bathymetric map (from GeoMapApp, www.geomapapp.org ), with main structural elements. Locations of major presalt anticline (Oceanus) and Tamar Gas Field are highlighted. (B) Regional cross section showing regional detachment within thick
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1973
AAPG Bulletin (1973) 57 (4): 637–641.
... springs occur along the line of this anticlinal. One of these is on the south side of the St. John River about half a mile above Douglastown. There the oil rises from the mud and shingle of the beach, and is seen in globules rising through the water at high tide. At both times it pollutes the sea...
FIGURES
Journal Article
Published: 30 January 2018
Journal of Sedimentary Research (2018) 88 (1): 148–176.
... ) in 1990 across the shelf and slope using a 120-channel, six-air-gun system with ∼ 10 m vertical resolution. This was followed by: 1) a higher-resolution, mid–outer shelf grid shot by the R/V Oceanus cruise Oc270 in 1995 using a single generator-injector (GI) gun and 48-channel HiRes equipment...
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Journal Article
Published: 01 September 1985
Journal of the Geological Society (1985) 142 (5): 815–836.
... van kalksteen gevormde depressie in het kong oppervlak van Banka, waarin een grote hoeveelheid tin erts is geaccumuleerd (mijn 7 der sectie Belinju) De Ingenieur in Indonesia 1950 2 6 16 Vail P. R. Hardebol J. Sea-level changes during the Tertiary Oceanus 1979 22 71 79 J...
Journal Article
Journal: AAPG Bulletin
Published: 01 March 1985
AAPG Bulletin (1985) 69 (3): 385–411.
... accumulated on the basin floor and terrigenous clastics were deposited on the eastern shelf, relatively undiluted diatomaceous deposits developed on outer shelves and slopes, atop anticlinal banks generated by wrench tectonism, and in some areas of the basin floor. A mid-Mohnian eustatic sea level rise caused...
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Journal Article
Journal: GSA Bulletin
Published: 01 May 2004
GSA Bulletin (2004) 116 (5-6): 594–605.
... to minimal erosion of the anticlinal fold surface, minimal sediment cover, and surface exposures that are unobstructed by vegetation. Additionally, thrust-related folds are distributed across the entire planet, within terranes of diverse origin and geologic history. The lithologic and volatile-induced...
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Journal Article
Journal: AAPG Bulletin
Published: 01 September 1995
AAPG Bulletin (1995) 79 (9): 1259–1273.
... structural and sedimentary styles, the Zagros foreland basin anticlines of shallow marine Precambrian to Pliocene rocks on the west and the Makran deep-water Eocene flysch belt on the east. A comparison of gravity features with surface structures on Thematic Mapper and Landsat Multispectral Scanner imagery...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1983
AAPG Bulletin (1983) 67 (7): 1143–1162.
.... Seismic reflection surveys and drilling followed, with anticlinal and reef plays being the dominant exploration prospects. Regional stratigraphy in and adjacent to the Central Valley has been described by Durkee and Pederson (1961) , Bandy (1963) , Amato (1965) , Roque et al (1972) , Ingle (1975...
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Journal Article
Published: 01 October 1997
Earth Sciences History (1997) 16 (2): 158–170.
... and London Clay, whereas number 4 extends south to the English Channel at Brighton across the great Weald anticline; curiously, the anticline is shown as if its crest were as angular as a roof ridgeline, whereas the London basin syncline is broadly curved. Section 2 extends southeast from Bath...
Journal Article
Journal: AAPG Bulletin
Published: 15 February 2020
AAPG Bulletin (2020) 104 (2): 411–448.
... data acquired from the research vessel (R/V) Oceanus expedition OC270 and well data from IODP expedition 313 ( Figure 2 ). The accuracy of the conversion of the seismic data (TWTT) to depth was checked against values obtained from OCS well velocity surveys at the well locations (check shot surveys...
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Journal Article
Journal: AAPG Bulletin
Published: 01 October 2011
AAPG Bulletin (2011) 95 (10): 1643–1666.
...) rimmed by the Claiborne Group (middle Eocene) strata. This uplift, probably middle Eocene in age, may well be caused by late Laramide compression from the southwest, as proposed by Laubach and Jackson (1990) , as coeval anticlines are formed in southwest Texas and northeastern Mexico ( Ewing, 2001...
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Journal Article
Journal: AAPG Bulletin
Published: 15 September 2019
AAPG Bulletin (2019) 103 (9): 2139–2175.
... rocks, migrated into a Neogene reservoir, and accumulated in an asymmetrical anticlinal structure ( Yin et al., 2007 ). To date, this oil field has produced more than 1.6 × 10 8 bbl of oil, with a recovery of more than 45% (W. L. Jiao, 2018, personal communication). At the end of the last century...
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Series: Geological Society, London, Special Publications
Published: 01 January 2015
DOI: 10.1144/SP401.22
EISBN: 9781862396777
... their counterparts on Mars and the Moon (e.g. Mueller & Golombek 2004 ), they are characterized by a steeply sloping scarp face and a gently sloping back limb (Fig. 3 d), and probably represent a monocline or asymmetrical hanging-wall anticline atop a blind or surface-breaking thrust fault. Mercury’s lobate...
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