Ige326
发表于 2025-3-25 06:05:42
Par Alain François Poignant4, is devoted to entropy. In particular, relative entropy, i.e., the entropy of one density relative to another, will be introduced and the maximum entropy principle will be discussed. In Sect. 2.5, the reader will meet the calculus of random variables; the central limit theorem in a first simple ve
d-limonene
发表于 2025-3-25 10:58:19
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HUSH
发表于 2025-3-25 13:51:07
Distribution of gastropods within the Cretaceous Tethyan realm same environments..Normally, marine gastropod assemblages of rocky surfaces or patches of hard substrates show high diversities of archaeogastropods. Level bottom communities are characterized by a high diversity of mesogastropods and cephalaspidean opisthobranchs. The evolution of neogastropods al
nocturnal
发表于 2025-3-25 19:32:35
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Constituent
发表于 2025-3-25 21:33:32
Tethys — the evolution of an ideahic conception, “Tethys” and “Tethyan” are currently used with different meanings in tectonics and paleo-biogeography. In paleobiogeography, Tethys is understood as a realm with varying extension. This dynamic conception is in contrast to the conception of the stable Cretaceous Mesogée by . (1900).
oblique
发表于 2025-3-26 02:03:20
The Lower Cretaceous Mésogée: A state of the arteous by applying advances in knowledge over the last 80 years to the original concept. The global distribution of rudist-orbitolinid assemblages support the broad configuration of Mésogée proposed by .. Their distribution is more extended than in the former definition, especially concerning the lati
和平主义
发表于 2025-3-26 07:21:33
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judiciousness
发表于 2025-3-26 08:34:44
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PET-scan
发表于 2025-3-26 15:19:25
Palaeogeographic distribution of Cretaceous Tethyan non-rudist bivalvesBarremian stage onwards with the spreading of the carbonate platform Tethyan faunas become more marked, with a rudist and a non-rudist facies. In the Albian a strong northern influence is visible in the northern Tethys. The successive Cenomanian transgressions result in a diversification of faunas;
考得
发表于 2025-3-26 18:50:15
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