Stratigraphy of the Neoproterozoic Damara Sequence in northwest Namibia: Slope to basin sub-marine mass-transport deposits and olistolith fields
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- 作者：D.B. Nascimentoa ; b ; debora@geologia.ufrj.br" class="auth_mail" title="E-mail the corresponding author ; A. Ribeirob ; andre@geologia.ufrj.br" class="auth_mail" title="E-mail the corresponding author ; R.A.J. Trouwb ; rajtrouw@hotmail.com" class="auth_mail" title="E-mail the corresponding author ; R.S. Schmittb ; renatagondwana@uol.com.br" class="auth_mail" title="E-mail the corresponding author ; C.W. Passchierc ; cpasschi@uni-mainz.de" class="auth_mail" title="E-mail the corresponding author
- 关键词：Deep-water deposits ; Olistolith ; Tectono-sequence ; Neoproterozoic ; Damara Sequence ; Namibia
- 刊名：Precambrian Research
- 出版年：2016
- 出版时间：June 2016
- 年：2016
- 卷：278
- 期：Complete
- 页码：108-125
- 全文大小：9774 K
文摘
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Slope to basin sub-marine mass-transport deposits in the Neoproterozoic Damara Sequence.
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Carbonate blocks and lenses interpreted as olistoliths.
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Sturtian and Marinoan units interpreted as gravity mass flow deposits.