Английская Википедия:Buildwas Formation

Материал из Онлайн справочника
Версия от 15:35, 12 февраля 2024; EducationBot (обсуждение | вклад) (Новая страница: «{{Английская Википедия/Панель перехода}} {{Use dmy dates|date=September 2019}} {{Infobox rockunit | name = Buildwas Formation<br>''formerly'' Wenlock Shale | image = | caption = | type = Formation | age = Sheinwoodian<br>{{fossil range|433.4|430.5}} | period = Sheinwoodian | prilithology = Mudstone | otherlithology = Limestone |...»)
(разн.) ← Предыдущая версия | Текущая версия (разн.) | Следующая версия → (разн.)
Перейти к навигацииПерейти к поиску

Шаблон:Use dmy dates Шаблон:Infobox rockunit

Файл:Laurasia 430Ma.jpg
Paleogeography of the Early Silurian, 430 Ma

The Buildwas Formation (Bw, BUI), formerly called Wenlock Shale and Buildwas Beds,[1] is a geologic formation in Shropshire, England. It preserves fossils dating back to the Silurian period. The formation is the defining formation of the Sheinwoodian age of the Wenlock epoch, the Middle Silurian.

Description

The Buildwas Formation comprises olive-green and grey calcareous mudstones and nodular to lenticular calcareous mudstones and argillaceous limestones with shell fragments present throughout. The basal part of the formation consists of grey-green rubbly mudstones, containing comminuted shell debris and overlies the mottled green, grey and purple mudstones of the Rubery Formation with a Шаблон:Convert thick transition in colour and upward decrease in number of hard siltstone beds. The top of the Buildwas Formation shows a gradational increase in thickness of beds and a number of limestone beds, where it grades into the overlying Barr Limestone Formation.

The thickness of the formation ranges from Шаблон:Convert, with the thinnest outcrops occurring near Walsall thickening towards Wenlock Edge. The type section of the formation was defined by Barrett in 1989 along the left (north) bank of Hughley Brook, Шаблон:Convert southeast of Leasows Farm and Шаблон:Convert northeast of Hughley Church.[1] The formation has provided fossils of Eodictyonella capewellii.[2]

See also

References

Шаблон:Reflist

Further reading

  • Bassett, M G, 1989. The Wenlock Series in the Wenlock area. 51-73 in "A global standard for the Silurian System". Holland, C H and Bassett, M G, (editors). National Museum of Wales, Gelogical series No.9, Cardiff.
  • A. D. Wright. 1981. The External Surface of Dictyonella and of other Pitted Brachiopods. Palaeontology 24(3):443-481
  • Basset, M G, 1974. Review of the stratigraphy of the Wenlock Series of the Welsh Borderlands and South Wales. Palaeontology, 17, 745-777.
  • Cocks, L R M, Holland, C H, Rickards, R B and Strachan, I, 1971. A correlation of Silurian rocks in the British Isles. Geological Society of London, Special Report No.1.
  • Butler, A J, 1937. On Silurian and Cambrian rocks encountered in a deep boring at Walsall, South Staffordshire, Geological Magazine, 74, 241-257.