Dynamic carbonate sedimentation on the Northern Line Islands Ridge, Palmyra Basin
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- 作者：Mitchell Lylea ; mlyle@coas.oregonstate.edu" class="auth_mail" title="E-mail the corresponding author ; Robert Pockalnyb ; rpockalny@uri.edu" class="auth_mail" title="E-mail the corresponding author ; Pratigya Polissarc ; polissar@ldeo.columbia.edu" class="auth_mail" title="E-mail the corresponding author ; Jean Lynch-Stieglitzd ; Jean@eas.gatech.edu" class="auth_mail" title="E-mail the corresponding author ; Samantha Bovae ; Samantha_Bova@Brown.edu" class="auth_mail" title="E-mail the corresponding author ; Ann G. Dunleaf ; adunlea@bu.edu" class="auth_mail" title="E-mail the corresponding author ; Heather Fordc ; hford@ldeo.columbia.edu" class="auth_mail" title="E-mail the corresponding author ; Jennifer E. Hertzbergg ; 1 ; jennifer.hertzberg@uconn.edu" class="auth_mail" title="E-mail the corresponding author ; Steven Hovanh ; hovan@iup.edu" class="auth_mail" title="E-mail the corresponding author ; Allison W. Jacobelc ; Jacobel@ldeo.columbia.edu" class="auth_mail" title="E-mail the corresponding author ; Christina King Wertmanb ; c_king@gso.uri.edu" class="auth_mail" title="E-mail the corresponding author ; Ashley E. Maloneyi ; ashjames@uw.edu" class="auth_mail" title="E-mail the corresponding author ; Richard W. Murrayf ; rickm@bu.edu" class="auth_mail" title="E-mail the corresponding author ; Julia Shackford Wilsong ; juliakwilson.13@gmail.com" class="auth_mail" title="E-mail the corresponding author ; Katherine Wejnertj ; katherine_e_wejnert@dekalbschoolsga.org" class="auth_mail" title="E-mail the corresponding author ; Ruifang C. Xiek ; ruifang.xie@mpic.de" class="auth_mail" title="E-mail the corresponding author
- 关键词：Central Pacific ; Carbonate sediments ; Line Islands Ridge ; Seismic stratigraphy ; Carbon cycle
- 刊名：Marine Geology
- 出版年：2016
- 出版时间：1 September 2016
- 年：2016
- 卷：379
- 期：Complete
- 页码：194-207
- 全文大小：5388 K
文摘
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Recent MGL1208 survey of Line Islands Ridge evaluates sedimentation on LIR.
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LIR and its apron add 5% to the equatorial Pacific carbonate province.
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Channels on LIR result from active erosion of pelagic carbonates to LIR apron.
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Strong currents on northern LIR forms foraminiferal sand waves in Palmyra Basin.
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Up to 1.3 km of sediment has accumulated since the late Cretaceous despite erosion.