Middle- Upper Ordovician shallow platform to deep basin transect, southern Tasmania, Australia

C. Burrett; B. Stait; C. Sharples; J. Laurie

Middle- Upper Ordovician shallow platform to deep basin transect, southern Tasmania, Australia

C. Burrett
, B. Stait
, C. Sharples
, J. Laurie

Research output: Contribution to journal › Article › peer-review

Abstract

There is a profound change in sedimentary environment and in fauna going from the Middle-Upper Ordovician of Ida Bay to Surprise Bay over a present distance of only 25 km. The transition is from peritidal carbonates at Ida Bay, to subtidal carbonates at Precipitous Bluff to deep subtidal calcareous shales at Pt. Cecil to deep water micrites, graptolitic shales and carbonate turbidites at Surprise Bay.-from Authors

Original language	English
Pages (from-to)	149-157
Number of pages	9
Journal	American Society of Mechanical Engineers (Paper)
Publication status	Published - 1984
Externally published	Yes

Cite this

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title = "Middle- Upper Ordovician shallow platform to deep basin transect, southern Tasmania, Australia",

abstract = "There is a profound change in sedimentary environment and in fauna going from the Middle-Upper Ordovician of Ida Bay to Surprise Bay over a present distance of only 25 km. The transition is from peritidal carbonates at Ida Bay, to subtidal carbonates at Precipitous Bluff to deep subtidal calcareous shales at Pt. Cecil to deep water micrites, graptolitic shales and carbonate turbidites at Surprise Bay.-from Authors",

author = "C. Burrett and B. Stait and C. Sharples and J. Laurie",

year = "1984",

language = "English",

pages = "149--157",

journal = "American Society of Mechanical Engineers (Paper)",

issn = "0402-1215",

publisher = "American Society of Mechanical Engineers (ASME)",

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TY - JOUR

T1 - Middle- Upper Ordovician shallow platform to deep basin transect, southern Tasmania, Australia

AU - Burrett, C.

AU - Stait, B.

AU - Sharples, C.

AU - Laurie, J.

PY - 1984

Y1 - 1984

N2 - There is a profound change in sedimentary environment and in fauna going from the Middle-Upper Ordovician of Ida Bay to Surprise Bay over a present distance of only 25 km. The transition is from peritidal carbonates at Ida Bay, to subtidal carbonates at Precipitous Bluff to deep subtidal calcareous shales at Pt. Cecil to deep water micrites, graptolitic shales and carbonate turbidites at Surprise Bay.-from Authors

AB - There is a profound change in sedimentary environment and in fauna going from the Middle-Upper Ordovician of Ida Bay to Surprise Bay over a present distance of only 25 km. The transition is from peritidal carbonates at Ida Bay, to subtidal carbonates at Precipitous Bluff to deep subtidal calcareous shales at Pt. Cecil to deep water micrites, graptolitic shales and carbonate turbidites at Surprise Bay.-from Authors

UR - https://www.scopus.com/pages/publications/0021577247

M3 - Article

AN - SCOPUS:0021577247

SN - 0402-1215

SP - 149

EP - 157

JO - American Society of Mechanical Engineers (Paper)

JF - American Society of Mechanical Engineers (Paper)

ER -

Middle- Upper Ordovician shallow platform to deep basin transect, southern Tasmania, Australia

Abstract

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