1-20 OF 26 RESULTS FOR

Dingo Gap

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Image
—Geologic map of the <b>Dingo</b> <b>Gap</b> area showing outcrop localities and measured...
Published: 01 November 2015
Fig. 6.— —Geologic map of the Dingo Gap area showing outcrop localities and measured section locations (modified after Playford et al. 2009 ). See Figure 1 for location along the Lennard Shelf. See Playton and Kerans (2015a) , Table 2 for explanation of formation names.
Image
FIGURE 4 —Microbial structures and renalcids from <b>Dingo</b> <b>Gap</b>. (A) Tracing of...
in > PALAIOS
Published: 01 June 2002
FIGURE 4 —Microbial structures and renalcids from Dingo Gap. (A) Tracing of thrombolite from polished hand sample. Notice the abundance of renalcids on pore tops. (B) Photomicrograph of thin section made from lower part of hand sample. Arrow points to dark renalcids on top of an interior pore
Journal Article
Published: 01 November 2015
Journal of Sedimentary Research (2015) 85 (11): 1362–1392.
...Fig. 6.— —Geologic map of the Dingo Gap area showing outcrop localities and measured section locations (modified after Playford et al. 2009 ). See Figure 1 for location along the Lennard Shelf. See Playton and Kerans (2015a) , Table 2 for explanation of formation names. ...
FIGURES | View All (21)
Image
Deposit types and features of Famennian middle-slope settings. See  Figures...
Published: 01 November 2015
outcrop photograph of megabreccia-filled channel with meter-scale blocks of reef-flat (rf), reef (r), and encrusted-upper-slope (us) material, DG4 Section, Dingo Gap area. Megabreccia matrix is quartz-rich grainstone, and channel incises several meters into platform-top-derived grainstones. gnstn
Image
Detailed architecture of silt- to grain-dominated Famennian middle-slope de...
Published: 01 November 2015
channel architecture of calcareous sandstones and quartz-rich oolitic grainstones within grain-dominated axis, DG1 Section, Dingo Gap area. C) Interpreted strike-view photomosaic of off-axis “gullied slope” architecture consisting of grain-rich to intraclastic gully and small-channel fills encased
Image
Schematic generalized models showing depositional, architectural, and syste...
Published: 01 November 2015
Fig. 9.— Schematic generalized models showing depositional, architectural, and systems-tract evolution across an interpreted Famennian high-frequency sequence, based on outcrops in the Windjana Gorge, Dingo Gap, and South Lawford Range (Casey Falls) areas. MFS, maximum flooding surface; SB
Journal Article
Journal: Geology
Published: 01 January 2017
Geology (2017) 45 (1): 7–10.
... . Images: NASA/JPL-Caltech/Malin Space Science Systems. Figure 3. Cylindrical structures at Dingo Gap and Marias Pass, Mars. A: Index image showing location of structures in B–F. B: Cylindrical structure. C: Close-up of wall of B, showing texture of rim. D: Deformational structure located 20 m...
Journal Article
Journal: PALAIOS
Published: 01 June 2002
PALAIOS (2002) 17 (3): 225–236.
...FIGURE 4 —Microbial structures and renalcids from Dingo Gap. (A) Tracing of thrombolite from polished hand sample. Notice the abundance of renalcids on pore tops. (B) Photomicrograph of thin section made from lower part of hand sample. Arrow points to dark renalcids on top of an interior pore...
FIGURES | View All (8)
Journal Article
Journal: AAPG Bulletin
Published: 01 June 1980
AAPG Bulletin (1980) 64 (6): 814–840.
... with the Devonian reefs of western Canada was made by Playford (1969) in collaboration with the Marathon Oil Co. Denver Research Center. More recently, detailed studies have been carried out by the Geological Survey in various key areas, notably at Bugle Gap, Windjana Gorge, Dingo Gap, and the northern Oscar...
FIGURES | View All (27)
Journal Article
Journal: Geology
Published: 01 April 2014
Geology (2014) 42 (4): 327–330.
... 13 C excursions in the Dingo Gap section; however, it is their broad upper excursion (composed of two distinct peaks) that corresponds to EX2 and EX3 based on conodont data ( George et al., 2013 ). Their upper peak is also in the Early triangularis Zone. Regionally, EX1–EX3 all coincide...
FIGURES
Journal Article
Published: 01 November 2015
Journal of Sedimentary Research (2015) 85 (11): 1334–1361.
... sections and slabs, and > 25 km 2 of detailed photomosaic and plan-view mapping from the South Lawford Range (Bugle Gap area), Dingo Gap, Windjana Gorge, and other localities in the Napier Range ( Fig. 1 ). The existing biostratigraphic framework (e.g., Becker et al. 1993 ; Becker and House 1997...
FIGURES | View All (17)
Series: Society for Sedimentary Geology
Publisher: Society for Sedimentary Geology
Published: 01 January 2017
DOI: 10.2110/sepmsp.106.05
EISBN: 9781565763456
.... Fig. 17. —Typical debris-flow megabreccia in fore-reef subfacies (Napier Formation) at Dingo Gap in the Napier Range. The megabreccia is composed of blocks of reef and reefal-slope limestones in a matrix of calcareous sandstone. Fig. 18. —Allochthonous block of reef limestone in fore-reef...
FIGURES | View All (43)
Journal Article
Published: 01 April 1982
Journal of the Geological Society (1982) 139 (2): 165–181.
... of northern Western Australia (with photographs from Dingo Gap and Winjana Gorge, courtesy of Playford), the Carboniferous (VisCan) bioherms (reef-knolls) near Clitheroe, Lanca- shire, England (Miller & Grayson 1972) and from Devonian exposures in Carrikre d s Croisettes, VodecCe, near Phillippeville, Belgium...
Journal Article
Journal: Interpretation
Published: 20 September 2019
Interpretation (2019) 7 (4): T773–T791.
...) measures, and reinterpretation. The same 13 horizons were interpreted on regional 2D seismic data within the WAMo polygon area to infill gaps in which 3D data were unavailable. The seismically derived horizons were then merged and gridded on a regular 50 × 50   m 2 mesh throughout...
FIGURES | View All (19)
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1970
AAPG Bulletin (1970) 54 (4): 583–600.
... and Tertiary geology of the continental shelf. Lack of deep seismic evidence inhibits detailed appreciation of pre-Mesozoic geology; this is mainly dependent on intuitive reasoning, based on a knowledge of the Precambrian and Paleozoic geology of the mainland of northwest Australia Gaps in the data...
FIGURES | View All (10)
Journal Article
Journal: Lithosphere
Published: 01 October 2015
Lithosphere (2015) 7 (5): 589–600.
... on a continental fragment that filled the current Cuvier Abyssal Plain gap, before breakup. Where did this fragment go? One solution is that this sliver drifted away with Greater India and was subsequently integrated in the Himalayan orogeny. However, Gibbons et al. (2012) proposed that the Sonja Ridge and Sonne...
FIGURES | View All (11)
Journal Article
Journal: AAPG Bulletin
Published: 01 July 2012
AAPG Bulletin (2012) 96 (7): 1369–1388.
... in the fracture network surrounding the dolomite bodies. (F) Limestone gap, or bridge, between two dolomite bodies. Much of the research involving the formation and characterization of hydrothermal dolomite reservoirs has involved an interpretation of subsurface data including well logs, seismic data...
FIGURES | View All (14)
Journal Article
Journal: AAPG Bulletin
Published: 01 September 2006
AAPG Bulletin (2006) 90 (9): 1359–1380.
... subbasins ( Figure 1 ). The Alpha Arch is the southerly extension of the Gorgon-Rankin high trend, which formed during Early Jurassic rifting ( Tindale et al., 1998 ; Workman et al., 2002 ). The Upper Jurassic Dingo claystone is believed to be the main oil-prone source rock for the region, based on oil...
FIGURES | View All (12)
Journal Article
Journal: Paleobiology
Published: 01 February 2011
Paleobiology (2011) 37 (1): 140–156.
... buttressing of cranial bones to withstand this stress, as well as a larger gap in the region of the bone-cracking teeth to increase the bending moment during the bone-cracking bite. The lack of accurate material properties for different-sized ungulate long bones prevents us from making absolute estimates...
FIGURES | View All (4)
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1985
AAPG Bulletin (1985) 69 (8): 1255–1268.
... Scarp and Leduc, from Devonian (age < 400 m.y.) rocks in Canada, already show abundant C 30 steranes. Perhaps we can fill this data gap by future analyses of additional lower Paleozoic samples. The C 28 -C 30 methyl steranes were found in both marine and nonmarine crudes. The presence of 4α...
FIGURES | View All (9)