A marine to fluvial transition in the the Paleoproterozoic Koolbye Formation, Turee Creek Group, Western Australia.

Although no unambiguous biogenic criteria exist to discriminate Precambrian shallow-marine successions from fluvial deposits, physical sedimentological evidence, including an association of primary sedimentary structures and textures, stratigraphic position, and comparison with Phanerozoic and Moder...

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Main Authors: Mazumder, Rajat, Van Kranendonk, M., Altermann, W.
Format: Journal Article
Published: Elsevier BV 2015
Online Access:http://hdl.handle.net/20.500.11937/10162
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author Mazumder, Rajat
Van Kranendonk, M.
Altermann, W.
author_facet Mazumder, Rajat
Van Kranendonk, M.
Altermann, W.
author_sort Mazumder, Rajat
building Curtin Institutional Repository
collection Online Access
description Although no unambiguous biogenic criteria exist to discriminate Precambrian shallow-marine successions from fluvial deposits, physical sedimentological evidence, including an association of primary sedimentary structures and textures, stratigraphic position, and comparison with Phanerozoic and Modern examples has been found useful in identifying these deposit types. Our high resolution sedimentary facies analysis coupled with new mapping clearly indicates shallow-marine to beach-aeolian to fluvial sedimentation in the Paleoproterozoic Koolbye Formation of the Turee Creek Group, Western Australia. A falling stage systems tract within the Koolbye Formation has been documented. Our sedimentary facies analysis in combination with sedimentological analysis of the underlying Kungarra Formation indicates development of at least three falling stage systems tracts within the Turee Creek Group across the rise of atmospheric oxygen (the Great oxidation event).
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format Journal Article
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institution Curtin University Malaysia
institution_category Local University
last_indexed 2025-11-14T06:28:46Z
publishDate 2015
publisher Elsevier BV
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spelling curtin-20.500.11937-101622018-03-29T09:05:56Z A marine to fluvial transition in the the Paleoproterozoic Koolbye Formation, Turee Creek Group, Western Australia. Mazumder, Rajat Van Kranendonk, M. Altermann, W. Although no unambiguous biogenic criteria exist to discriminate Precambrian shallow-marine successions from fluvial deposits, physical sedimentological evidence, including an association of primary sedimentary structures and textures, stratigraphic position, and comparison with Phanerozoic and Modern examples has been found useful in identifying these deposit types. Our high resolution sedimentary facies analysis coupled with new mapping clearly indicates shallow-marine to beach-aeolian to fluvial sedimentation in the Paleoproterozoic Koolbye Formation of the Turee Creek Group, Western Australia. A falling stage systems tract within the Koolbye Formation has been documented. Our sedimentary facies analysis in combination with sedimentological analysis of the underlying Kungarra Formation indicates development of at least three falling stage systems tracts within the Turee Creek Group across the rise of atmospheric oxygen (the Great oxidation event). 2015 Journal Article http://hdl.handle.net/20.500.11937/10162 10.1016/j.precamres.2014.12.005 Elsevier BV restricted
spellingShingle Mazumder, Rajat
Van Kranendonk, M.
Altermann, W.
A marine to fluvial transition in the the Paleoproterozoic Koolbye Formation, Turee Creek Group, Western Australia.
title A marine to fluvial transition in the the Paleoproterozoic Koolbye Formation, Turee Creek Group, Western Australia.
title_full A marine to fluvial transition in the the Paleoproterozoic Koolbye Formation, Turee Creek Group, Western Australia.
title_fullStr A marine to fluvial transition in the the Paleoproterozoic Koolbye Formation, Turee Creek Group, Western Australia.
title_full_unstemmed A marine to fluvial transition in the the Paleoproterozoic Koolbye Formation, Turee Creek Group, Western Australia.
title_short A marine to fluvial transition in the the Paleoproterozoic Koolbye Formation, Turee Creek Group, Western Australia.
title_sort marine to fluvial transition in the the paleoproterozoic koolbye formation, turee creek group, western australia.
url http://hdl.handle.net/20.500.11937/10162