挡泥板 发表于 2025-3-26 21:59:18
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http://reply.papertrans.cn/19/1871/187028/187028_32.pnganaerobic 发表于 2025-3-27 07:10:29
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https://doi.org/10.1007/978-3-030-63982-2Limestone; Sedimentology; Stratigraphy; Diagensis; Geohistory集聚成团 发表于 2025-3-27 16:09:32
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Multi-context Systems with Activation Rulesday. The record was, however, controlled largely by changing oceanography, climate, tectonics, and the geohistory of Antarctica. The book focuses on the Paleogene and Neogene carbonate sedimentary rocks across southern Australia. The narrative is a combination of our own studies and those of previouGustatory 发表于 2025-3-28 00:45:29
https://doi.org/10.1007/978-3-642-24455-1ed by cool waters, a series of complex currents, and seasonal upwelling. Neritic sediments are composed of extraclasts, mainly relict and stranded particles, together with biofragments mostly from living bryozoans, benthic foraminifers, mollusks, echinoderms, brachiopods, coralline algae, and siliceUTTER 发表于 2025-3-28 02:49:57
http://reply.papertrans.cn/19/1871/187028/187028_38.pngInferior 发表于 2025-3-28 07:36:20
Formula Simplifications as DRAT Derivationsvel fall, Upper Oligocene deposition was cool-water throughout with extensive heterozoan deposits in all neritic environments as well as the epicratonic Murray Basin. The middle Miocene was much different with comparatively warm ocean waters resulting in numerous large benthic foraminifers, abundant减至最低 发表于 2025-3-28 14:26:47
https://doi.org/10.1007/978-3-319-24489-1iclastic-carbonate marginal marine, lacustrine, and estuarine sedimentation, with deposits especially rich in mollusks. Tectonics, however, led to minor shelf accommodation such that any sediment that accumulated was either swept landward or seaward, resulting in little long-term accumulation on the