碌碌之人
发表于 2025-3-25 05:49:40
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eardrum
发表于 2025-3-25 07:32:04
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prostatitis
发表于 2025-3-25 12:55:33
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以烟熏消毒
发表于 2025-3-25 18:59:30
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inspiration
发表于 2025-3-25 21:56:25
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POINT
发表于 2025-3-26 00:20:36
The Modern Carbonate Depositional Realmed 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 silice
嘴唇可修剪
发表于 2025-3-26 08:10:30
Succession SA2: Middle Eocene to Lower Oligocene—‘The Biogenic Shelf’ ~ 43-28 Maest but by the early Oligocene extended into the Otway Basin. SA2.1—Middle Eocene strata, are largely marginal, inner, and mid neritic siliciclastics passing outboard into carbonates with deep water bryozoan mounds. SA2.2—Mid to Upper Eocene rocks are mostly similar with carbonaceous inboard terrest
CROW
发表于 2025-3-26 10:47:29
Succession SA3: Late Oligocene—Middle Miocene—‘The Carbonate Shelf’ ~28–11 Mavel 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
植物学
发表于 2025-3-26 16:18:41
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相信
发表于 2025-3-26 19:44:28
Diagenesismargin subsidence was largely characterized by seafloor carbonate dissolution, omission surface precipitation (hardgrounds) and burial alteration, there was no significant meteoric alteration. This latter aspect was largely due to the fact that there were few aragonitic components in the sediment an