Hyperpycnal transport of carbonaceous sediment - Example from the Upper Devonian Rhinestreet Shale, western New York, U.S.A.
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- 作者：Gary G. Lash Lash@fredonia.edu" class="auth_mail" title="E-mail the corresponding author
- 关键词：Black shale ; Appalachian Basin ; Hyperpycnite ; Burn down ; Monsoon
- 刊名：Palaeogeography, Palaeoclimatology, Palaeoecology
- 出版年：2016
- 出版时间：1 October 2016
- 年：2016
- 卷：459
- 期：Complete
- 页码：29-43
- 全文大小：3929 K
文摘
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Upper Devonian black shale layers accumulated from hyperpycnal flows.
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Hyperpycnal turbidity currents were generated during periods of wetter climate.
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Hyperpycnal flows transported organic debris to cratonic basinal environments.
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Hyperpycnites appear to have been diagenetically altered by burn down.