Lithology and characteristics of the Messinian evaporite sequence of the deep Levant Basin, eastern Mediterranean
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- 作者：Ye E. Fenga ; yefeng@post.tau.ac.il" class="auth_mail" title="E-mail the corresponding author ; Anastasya Yankelzona ; Josh Steinbergb ; Moshe Reshefa
- 关键词：Messinian Salinity Crisis ; Levant Basin ; Well log interpretation ; Lithology ; Evaporite stratigraphy ; Salt deformation
- 刊名：Marine Geology
- 出版年：2016
- 出版时间：1 June 2016
- 年：2016
- 卷：376
- 期：Complete
- 页码：118-131
- 全文大小：7602 K
文摘
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We present previously unreleased 3D PSDM seismic and deepwater industry well log data.
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Seismic transparent units are composed of pure and uniform halite.
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Seismic reflective units comprise thin clastic layers interbedded in halite.
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Clastic units were likely transported into the deep Levant Basin.
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We present geometry of intra-evaporite units and their deformation characteristics.