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Minchinbury Sandstone

Triassic age unit of sedimentary rock in Australia


Triassic age unit of sedimentary rock in Australia

FieldValue
nameMinchinbury Sandstone
periodMiddle Triassic
age
imageSandstone beside Duck River NSW.JPG
captionExposed sandstone beside the Duck River, in South Granville
typeGeological formation
prilithologySandstone
otherlithologyShale
unitofWiannamatta group
underliesBringelly Shale
overliesHawkesbury sandstone
thicknessup to 6 m
locationSydney, Australia
regionWestern Sydney, south-western Sydney
countryAustralia
namedforMinchinbury
namedby
year_ts
location_ts
coordinates_ts
paleocoordinates_ts
region_ts
country_ts
thickness_ts

Minchinbury Sandstone is a component of the Wianammatta Group of sedimentary rocks in the Sydney Basin of eastern Australia that was formed in the middle Triassic period. The sandstone was structured by marine deposition as a set of sandy barrier islands at a coastal shoreline.

Description

Thickness is between 1.5 m and 6 m , usually less than 3 m . It comprises up to 70% quartz with calcite and volcanic lithic fragments. There is less feldspar and more calcite than the adjacent Bringelly Shale. Related to Greywacke, it comprises fine to medium-grained lithic sandstone. The sandstone is a shoreline facies containing a beach and barrier bar complex.

The Bringelly Shale lies above the Minchinbury Sandstone. Fossils are rare in this stratum, though plant fragments have been recorded.

Location

The type locality of the formation is near the Great Western Highway in the suburb of Minchinbury in western Sydney. It is most often seen in the western parts of the city. Outcroppings are weak and not easily found, but it may be seen in places like road cuttings in localities from Epping, Grose Vale-Kurrajong, Kellyville, Rogans Hill, Bankstown, Pendle Hill, Bonnyrigg, Menangle, Duck River, Brownlow Hill and other sites.

At Minchinbury, the sandstone is more than 100 m deep in a downhole, and its natural outcrops are particularly elusive to find elsewhere. In Lansdowne, there are large, albeit disconnected sandstone slabs, with other smaller outcrops and floaters dispersed near a slope.

References

References

  1. (1980). "A Guide to the Sydney basin". Geological Survey of NSW.
  2. John Byrnes & [[Viera Scheibner]]. "The inorganic nature of marine microfossils described from the Wianamatta Group". Geological Survey of New South Wales.
  3. "Bulletin No. 25 - 1979: The Geology and Resource Potential of the Wianamatta Group.". [[New South Wales Government]].
  4. "Geology Of The Triassic Rocks Of The Sydney Area". pellsconsulting.com.au.
  5. "Minchinbury Sandstone". Australian Government.
  6. Lovering, J. F., 1954. "Bringelly Shale". Australian Museum.
  7. "Wianamatta Group". Step.org.
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