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Titlebook: Geology of Cuba; Manuel Enrique Pardo Echarte Book 2021 Springer Nature Switzerland AG 2021 Cuban Geology.Geological Cartography.Marine Ge

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樓主: firearm
31#
發(fā)表于 2025-3-26 22:27:44 | 只看該作者
2364-6438 of Cuba, which covers approximately the last 200 million years of life on Earth, is rich in very varied fossils, witnessing a wide diversity of organisms, both animals and pl978-3-030-67800-5978-3-030-67798-5Series ISSN 2364-6438 Series E-ISSN 2364-6446
32#
發(fā)表于 2025-3-27 02:08:39 | 只看該作者
33#
發(fā)表于 2025-3-27 06:21:34 | 只看該作者
978-3-030-67800-5Springer Nature Switzerland AG 2021
34#
發(fā)表于 2025-3-27 11:49:17 | 只看該作者
35#
發(fā)表于 2025-3-27 17:36:06 | 只看該作者
36#
發(fā)表于 2025-3-27 18:19:03 | 只看該作者
37#
發(fā)表于 2025-3-27 21:57:22 | 只看該作者
Digital Business als neue Unternehmensformthe upper edge of the insular slope and the current coast. The investigations reveal that the deposits of this interval have different characteristics to those of the emerged territories of the islands of Cuba and of de la Juventud, determined by: (1) their biogenic-carbonate composition without or
38#
發(fā)表于 2025-3-28 04:28:31 | 只看該作者
Die Grundlagen des Digital Business,ing a wide diversity of organisms, both animals and plants, that inhabited the Antillean and Caribbean region and constitute the inheritance of the biological diversity exhibited by the current Cuban Archipelago. The most characteristic fossils of Jurassic Period in Cuba are petrified bones of marin
39#
發(fā)表于 2025-3-28 09:06:56 | 只看該作者
Preconditions of Digital Engagement of the Cuban archipelago. Precambrian rocks have been dated to singular outcrops in the southern area of Corralillo and La Teja in the provinces of Villa Clara and Matanzas, respectively. The formations of these periods are represented by sedimentary, volcanic, volcanic-sedimentary, and metamorphic
40#
發(fā)表于 2025-3-28 13:39:51 | 只看該作者
Clinical applications of cardiac CTmainly formed by Jurassic–Eocene rocks, unconformably resting below the cover. The socle is divided into three major complexes, according to their litho-structural features and rock age: (a) the Proterozoic–Paleozoic basement, (b) the Mesozoic basement, and (c) the Paleogene folded and thrust belt.
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