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Titlebook: Evaporite Basins; Tadeusz M. Peryt Book 1987 Springer-Verlag Berlin Heidelberg 1987 Deformation.Sediment.Trias.diagenesis.environment.form

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發(fā)表于 2025-3-21 19:20:24 | 只看該作者 |倒序瀏覽 |閱讀模式
書目名稱Evaporite Basins
編輯Tadeusz M. Peryt
視頻videohttp://file.papertrans.cn/318/317398/317398.mp4
叢書名稱Lecture Notes in Earth Sciences
圖書封面Titlebook: Evaporite Basins;  Tadeusz M. Peryt Book 1987 Springer-Verlag Berlin Heidelberg 1987 Deformation.Sediment.Trias.diagenesis.environment.form
出版日期Book 1987
關(guān)鍵詞Deformation; Sediment; Trias; diagenesis; environment; formation
版次1
doihttps://doi.org/10.1007/BFb0010095
isbn_softcover978-3-540-18679-3
isbn_ebook978-3-540-48069-3Series ISSN 0930-0317 Series E-ISSN 1613-2580
issn_series 0930-0317
copyrightSpringer-Verlag Berlin Heidelberg 1987
The information of publication is updating

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沙發(fā)
發(fā)表于 2025-3-22 00:19:12 | 只看該作者
Depositional models of lower and middle triassic evaporites in the upper Yangtze area, China,ological setting and the development of evaporites suggest that the basins were flat and shallow, and were formed in two ways: one is to develop in the progradational-coastal sabkha were seaside depressions formed by subsidence, the other, relic lake formed in inner shelf depressions by rapid regres
板凳
發(fā)表于 2025-3-22 03:48:36 | 只看該作者
Middle muschelkalk evaporitic deposits in eastern Paris basin,ontinental influences on evaporitic sedimentation: fresh water and detrital supplies, and salt dissolution. More or less evaporated sea water flowing into the basin causes a cyclic evolution of salinity throughout the series..The deposit is generally layered and shows millimetric to centimetric prim
地板
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https://doi.org/10.1007/978-1-4757-5070-6ontinental influences on evaporitic sedimentation: fresh water and detrital supplies, and salt dissolution. More or less evaporated sea water flowing into the basin causes a cyclic evolution of salinity throughout the series..The deposit is generally layered and shows millimetric to centimetric prim
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發(fā)表于 2025-3-23 00:51:05 | 只看該作者
https://doi.org/10.1007/BFb0010095Deformation; Sediment; Trias; diagenesis; environment; formation
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Evaporite Basins978-3-540-48069-3Series ISSN 0930-0317 Series E-ISSN 1613-2580
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