Sedimentary fabrics of the macrotidal, mud-dominated, inner estuary to fluvio-tidal transition zone, Petitcodiac River estuary, New Brunswick, Canada
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- 作者：Alina Shchepetkina ; shchepet@ualberta.ca" class="auth_mail" title="E-mail the corresponding author ; Murray K. Gingras ; John-Paul Zonneveld ; S. George Pemberton
- 关键词：Fine-grained sedimentation ; Fluvio-tidal transition ; Sedimentary structures ; Ichnology ; Petitcodiac River estuary
- 刊名：Sedimentary Geology
- 出版年：2016
- 出版时间：15 March 2016
- 年：2016
- 卷：333
- 期：Complete
- 页码：147-163
- 全文大小：5308 K
文摘
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Description of mud-dominated sedimentary fabrics, application for the rock record.
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Facies distribution of the clay- and silt-rich deposits.
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Inner estuary locale - thick accumulations of interbedded silt and silty clay (IHS).
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Fluvio-tidal transition zone - interbedded sand and gravel with silty mud.
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The fluvial reach – massive to cross-stratified gravel – and granule-bed deposits