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![—Detailed section through <span class="search-highlight">Arumbera</span> <span class="search-highlight">Sandstone</span> in Ooraminna subbasin (134°29’...]()
![—Isopach map of <span class="search-highlight">Arumbera</span> <span class="search-highlight">Sandstone</span> showing areas of progradation and oniap ...]()
![—Histogram of <span class="search-highlight">Arumbera</span> <span class="search-highlight">Sandstone</span> thickness based on seismic data. Tliicknes...]()
![—Distribution of Bitter Springs Formation salt beneatii <span class="search-highlight">Arumbera</span> <span class="search-highlight">Sandstone</span>....]()
![—Two-way time to top of <span class="search-highlight">Arumbera</span> <span class="search-highlight">Sandstone</span>. C.I. = 250 msec. Contours based...]()
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![—Idealized north-south cross sections through A A’ Carmichael subbasin, BB’...]()
![—Histogram of thickness of <span class="search-highlight">sandstone</span> beds interpreted as turbidites within ...]()
![—Contours showing frequency distribution of seismic reflectors internal to ...]()
![—Areal photograph taken approximately 500 m above the ground showing (1) Ju...]()
![—Seismic line 81-Ul across western margin of Carmicliael subbasin, showing ...]()
![Sole marks in Phanerozoic shallow marine successions. A: Groove casts and p...]()
![Tera–Wasserburg concordia diagram for zircon from ( a ) Irindina Gneiss met...]()
![ε Nd v. time plots for Officer Basin samples. Included are the ε Nd va...]()
![Probability distribution diagrams for the ages of detrital zircons from: ( ...]()
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![Global Arumberia examples. (a) Maturin Ponds Formation, Canada. Note freq...]()
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1-20 OF 51 RESULTS FOR
Arumbera Sandstone
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Journal Article
Arumbera Sandstone: A Possible Late Proterozoic-Early Cambrian Deltaic Complex, Central Australia: ABSTRACT
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 01 May 1982
AAPG Bulletin (1982) 66 (5): 559.
...Keith T. Conrad; Robert Q. Oaks, Jr. A detailed investigation of the Arumbera Sandstone was undertaken in the northeastern Amadeus basin, central Australia, where the unit forms distinctive strike ridges with orange-white cliffs and dark reddish slopes. The Arumbera is divisible into four informal...
Image
—Detailed section through Arumbera Sandstone in Ooraminna subbasin (134°29’...
in Sequence Stratigraphy and Depositional Controls in Late Proterozoic-Early Cambrian Sediments of Amadeus Basin, Central Australia
> AAPG Bulletin
Published: 01 November 1987
Figure 4 —Detailed section through Arumbera Sandstone in Ooraminna subbasin (134°29’E, 23°36’S) showing two depositional sequences and interpreted facies associations. At this locality, sequence 2 is relatively thin compared with its development closer to center of subbasin. HCS = hummocky cross
Image
—Isopach map of Arumbera Sandstone showing areas of progradation and oniap ...
in Sequence Stratigraphy and Depositional Controls in Late Proterozoic-Early Cambrian Sediments of Amadeus Basin, Central Australia
> AAPG Bulletin
Published: 01 November 1987
Figure 10 —Isopach map of Arumbera Sandstone showing areas of progradation and oniap and location of Bitter Springs Formation salt highs. CI. = 100 m. Beyond seismic network to east of Alice Springs, isopachs are based on field observations made during present study and earlier field programs
Image
—Histogram of Arumbera Sandstone thickness based on seismic data. Tliicknes...
in Sequence Stratigraphy and Depositional Controls in Late Proterozoic-Early Cambrian Sediments of Amadeus Basin, Central Australia
> AAPG Bulletin
Published: 01 November 1987
Figure 11 —Histogram of Arumbera Sandstone thickness based on seismic data. Tliickness of formation was determined at 783 shot-point locations.
Image
—Distribution of Bitter Springs Formation salt beneatii Arumbera Sandstone....
in Sequence Stratigraphy and Depositional Controls in Late Proterozoic-Early Cambrian Sediments of Amadeus Basin, Central Australia
> AAPG Bulletin
Published: 01 November 1987
Figure 17 —Distribution of Bitter Springs Formation salt beneatii Arumbera Sandstone. In general, salt is thickest beneath areas where Arumbera Sandstone is thin.
Image
—Two-way time to top of Arumbera Sandstone. C.I. = 250 msec. Contours based...
in Sequence Stratigraphy and Depositional Controls in Late Proterozoic-Early Cambrian Sediments of Amadeus Basin, Central Australia
> AAPG Bulletin
Published: 01 November 1987
Figure 9 —Two-way time to top of Arumbera Sandstone. C.I. = 250 msec. Contours based on local seismic datum: 550 m above sea level.
Journal Article
Sequence Stratigraphy and Depositional Controls in Late Proterozoic-Early Cambrian Sediments of Amadeus Basin, Central Australia
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 01 November 1987
AAPG Bulletin (1987) 71 (11): 1387–1403.
...Figure 4 —Detailed section through Arumbera Sandstone in Ooraminna subbasin (134°29’E, 23°36’S) showing two depositional sequences and interpreted facies associations. At this locality, sequence 2 is relatively thin compared with its development closer to center of subbasin. HCS = hummocky cross...
FIGURES
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Journal Article
Salt-Induced Growth Structures and Subsequent Overthrusts, Northeastern Amadeus Basin, Central Australia: ABSTRACT
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 01 May 1982
AAPG Bulletin (1982) 66 (5): 614–615.
...Robert Q. Oaks, Jr.; Keith T. Conrad*; James A. Deckelman Thicknesses of the late Proterozoic-Early Cambrian Arumbera Sandstone and Middle Cambrian Giles Creek Formation show initiation of growth of the Brumby anticline during the Middle Cambrian. Growth probably resulted from flowage of bedded...
Image
—Idealized north-south cross sections through A A’ Carmichael subbasin, BB’...
in Sequence Stratigraphy and Depositional Controls in Late Proterozoic-Early Cambrian Sediments of Amadeus Basin, Central Australia
> AAPG Bulletin
Published: 01 November 1987
Figure 16 —Idealized north-south cross sections through A A’ Carmichael subbasin, BB’ Missionary Plains trough, and CC’ the Ooraminna subbasin, showing relationship between two depositional sequences within Arumbera Sandstone and relationship of formation to underlying Bitter Springs
Image
—Histogram of thickness of sandstone beds interpreted as turbidites within ...
in Sequence Stratigraphy and Depositional Controls in Late Proterozoic-Early Cambrian Sediments of Amadeus Basin, Central Australia
> AAPG Bulletin
Published: 01 November 1987
Figure 6 —Histogram of thickness of sandstone beds interpreted as turbidites within pelagic unit at base of sequence 1 of Arumbera Sandstone in Missionary Plains trough.
Image
—Contours showing frequency distribution of seismic reflectors internal to ...
in Sequence Stratigraphy and Depositional Controls in Late Proterozoic-Early Cambrian Sediments of Amadeus Basin, Central Australia
> AAPG Bulletin
Published: 01 November 1987
Figure 13 —Contours showing frequency distribution of seismic reflectors internal to Arumbera Sandstone. C.I. = 2. Note that reflector numbers increase in basinward direction from areas of progradation and in areas of basal onlap.
Image
—Areal photograph taken approximately 500 m above the ground showing (1) Ju...
in Sequence Stratigraphy and Depositional Controls in Late Proterozoic-Early Cambrian Sediments of Amadeus Basin, Central Australia
> AAPG Bulletin
Published: 01 November 1987
Figure 5 —Areal photograph taken approximately 500 m above the ground showing (1) Julie Formation, (2) sequence 1, and (3) sequence 2 of Arumbera Sandstone in the Ooraminna subbasin 50 km east of Alice Springs.
Image
—Seismic line 81-Ul across western margin of Carmicliael subbasin, showing ...
in Sequence Stratigraphy and Depositional Controls in Late Proterozoic-Early Cambrian Sediments of Amadeus Basin, Central Australia
> AAPG Bulletin
Published: 01 November 1987
Figure 14 —Seismic line 81-Ul across western margin of Carmicliael subbasin, showing two sequences within Arumbera Sandstone. Boundary between two sequences appears to be Proterozoic-Cambrian boundary. See Figure 8 for location of line.
Image
Sole marks in Phanerozoic shallow marine successions. A: Groove casts and p...
Published: 01 August 2018
, millimeter-scale, parallel to subparallel groove casts, Cambrian Arumbera Sandstone (Australia; 23°35.727’S, 134°22.698’E). D: Crisply preserved groove casts (white arrows) and prod marks (black-rimmed white arrows) of millimeter-scale diameter, associated with horizontal burrows and arthropodal scratch
Image
Tera–Wasserburg concordia diagram for zircon from ( a ) Irindina Gneiss met...
in Detrital zircon provenance constraints on the evolution of the Harts Range Metamorphic Complex (central Australia): links to the Centralian Superbasin
> Journal of the Geological Society
Published: 01 September 2005
Metamorphic Complex; ( d ) Arumbera Sandstone sample 93-1173, Amadeus Basin; ( e ) Pacoota Sandstone sample 93-1407, Amadeus Basin. The insets show the relative probability distribution of ages obtained from detrital zircons. These diagrams were constructed using 207 Pb/ 206 Pb ages for apparent age
Image
ε Nd v. time plots for Officer Basin samples. Included are the ε Nd va...
in Nd isotopic and geochemical constraints on provenance of sedimentary rocks in the eastern Officer Basin, Australia: implications for the duration of the intracratonic Petermann Orogeny
> Journal of the Geological Society
Published: 01 May 2005
Fig. 8. ε Nd v. time plots for Officer Basin samples. Included are the ε Nd values for the Arumbera Sandstone plotted as stars ( ε Nd is −9.2 and −8.8 at 600 Ma) ( Zhao et al . 1992 ). Average basement data are plotted for the Musgrave Block (Musgrave Block (average of 20 data points
Image
Probability distribution diagrams for the ages of detrital zircons from: ( ...
in Detrital zircon provenance constraints on the evolution of the Harts Range Metamorphic Complex (central Australia): links to the Centralian Superbasin
> Journal of the Geological Society
Published: 01 September 2005
, all from the Mallee Bore area of the NW Harts Range ( Buick et al . 2001 ); ( h ) average Arunta Inlier and the Musgrave Inlier sources ( Camacho et al . 2002 ), ( i ) the Pacoota Sandstone (this study), ( j ) the Goyder Formation ( Zhao et al . 1992 ), ( k ) the Arumbera Sandstone (this study
Journal Article
Rapid Early Cambrian rotation of Gondwana
Journal: Geology
Publisher: Geological Society of America
Published: 01 August 2010
Geology (2010) 38 (8): 755–758.
... samples from all three formations—Arumbera Sandstone, Hugh River Shale, and Jay Creek Limestone—shared two broadly similar magnetic components: a low-stability component coincident with the present local geocentric axial dipole field, and a high-stability component of varying orientations. Alternating...
FIGURES
Image
Global Arumberia examples. (a) Maturin Ponds Formation, Canada. Note freq...
in Enigma variations: characteristics and likely origin of the problematic surface texture Arumberia , as recognized from an exceptional bedding plane exposure and the global record
> Geological Magazine
Published: 17 September 2021
diameter of 16.25 mm. (e) Synalds Formation, United Kingdom. (f) Crown Hill Formation, Canada. In this instance Arumberia lines follow the direction indicated by the underlying linguoid ripple marks. Coin has diameter of 16.25 mm. (g) Arumbera Sandstone, Australia. (h) Maturin Ponds Formation, Canada
Journal Article
Detrital zircon provenance constraints on the evolution of the Harts Range Metamorphic Complex (central Australia): links to the Centralian Superbasin
Journal: Journal of the Geological Society
Publisher: Geological Society of London
Published: 01 September 2005
Journal of the Geological Society (2005) 162 (5): 777–787.
... Metamorphic Complex; ( d ) Arumbera Sandstone sample 93-1173, Amadeus Basin; ( e ) Pacoota Sandstone sample 93-1407, Amadeus Basin. The insets show the relative probability distribution of ages obtained from detrital zircons. These diagrams were constructed using 207 Pb/ 206 Pb ages for apparent age...
FIGURES
| View All (5)
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