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Titlebook: Recent Developments in High-Speed Transport; Selected Contributio Dmitry Yu. Strelets,Oleg N. Korsun Book 2023 The Editor(s) (if applicable

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21#
發(fā)表于 2025-3-25 04:17:40 | 只看該作者
O. N. Korsun,A. A. Pirozhkov,E. D. Glukhova,N. V. Skryabikov scale and the evolution at a larger sequential scale depends upon which one of these factors becomes dominant. The general evolution results in a typical sedimentary cycle..The structural behavior of the Hercynian basement controls distribution and sometimes preservation of the depsits. Diagenesis
22#
發(fā)表于 2025-3-25 08:15:42 | 只看該作者
23#
發(fā)表于 2025-3-25 15:28:06 | 只看該作者
A. Y. Grishina,A. V. Efremov scale and the evolution at a larger sequential scale depends upon which one of these factors becomes dominant. The general evolution results in a typical sedimentary cycle..The structural behavior of the Hercynian basement controls distribution and sometimes preservation of the depsits. Diagenesis
24#
發(fā)表于 2025-3-25 18:46:11 | 只看該作者
V. A. Prodanik,A. V. Efremov scale and the evolution at a larger sequential scale depends upon which one of these factors becomes dominant. The general evolution results in a typical sedimentary cycle..The structural behavior of the Hercynian basement controls distribution and sometimes preservation of the depsits. Diagenesis
25#
發(fā)表于 2025-3-25 20:43:30 | 只看該作者
26#
發(fā)表于 2025-3-26 01:39:51 | 只看該作者
O. N. Korsun,S. V. Nikolaev,M. H. Om scale and the evolution at a larger sequential scale depends upon which one of these factors becomes dominant. The general evolution results in a typical sedimentary cycle..The structural behavior of the Hercynian basement controls distribution and sometimes preservation of the depsits. Diagenesis
27#
發(fā)表于 2025-3-26 05:58:43 | 只看該作者
28#
發(fā)表于 2025-3-26 11:16:57 | 只看該作者
29#
發(fā)表于 2025-3-26 15:20:26 | 只看該作者
30#
發(fā)表于 2025-3-26 17:52:57 | 只看該作者
o diapirs and welds (halokinetic breccias) or have acted as décollement surfaces in fold and thrust belts (rauhwacke). All evaporite salt units will ultimately dissolve, many disappear in the diagenetic realm while others may be preserved until they attain metamorphic grades or interact with a magma
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