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Titlebook: Evolution of the Mid-Cretaceous Triad; Platform Carbonates, Karl B. Follmi Book 1989 Springer-Verlag Berlin Heidelberg 1989 Cretaceous.Detr

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發(fā)表于 2025-3-21 18:29:54 | 只看該作者 |倒序瀏覽 |閱讀模式
書目名稱Evolution of the Mid-Cretaceous Triad
副標(biāo)題Platform Carbonates,
編輯Karl B. Follmi
視頻videohttp://file.papertrans.cn/318/317781/317781.mp4
叢書名稱Lecture Notes in Earth Sciences
圖書封面Titlebook: Evolution of the Mid-Cretaceous Triad; Platform Carbonates, Karl B. Follmi Book 1989 Springer-Verlag Berlin Heidelberg 1989 Cretaceous.Detr
描述Paleoceanographic conditions which led to the formation of the "mid"-cretaceous triad along the northern Tethys margin are elucidated. In the first part, the evolution of this sequence is traced from the demise of the platform to the return of the detritus dominated deposition. The second part includes a discussion of the reconstructed paleoceanographic and tectonic variables, their possible interaction as well as their influence on sediment properties.
出版日期Book 1989
關(guān)鍵詞Cretaceous; Detritus; Sediment; evolution; ocean
版次1
doihttps://doi.org/10.1007/BFb0019667
isbn_softcover978-3-540-51359-9
isbn_ebook978-3-540-46199-9Series ISSN 0930-0317 Series E-ISSN 1613-2580
issn_series 0930-0317
copyrightSpringer-Verlag Berlin Heidelberg 1989
The information of publication is updating

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發(fā)表于 2025-3-21 23:59:47 | 只看該作者
Book 1989rt, the evolution of this sequence is traced from the demise of the platform to the return of the detritus dominated deposition. The second part includes a discussion of the reconstructed paleoceanographic and tectonic variables, their possible interaction as well as their influence on sediment properties.
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0930-0317 part includes a discussion of the reconstructed paleoceanographic and tectonic variables, their possible interaction as well as their influence on sediment properties.978-3-540-51359-9978-3-540-46199-9Series ISSN 0930-0317 Series E-ISSN 1613-2580
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Book 1989rt, the evolution of this sequence is traced from the demise of the platform to the return of the detritus dominated deposition. The second part includes a discussion of the reconstructed paleoceanographic and tectonic variables, their possible interaction as well as their influence on sediment prop
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