Titlebook: Biogenic Sedimentary Rocks in a Cold, Cenozoic Ocean; Neritic Southern Aus Noel P. James,Yvonne Bone Book 2021 The Editor(s) (if applicable

擋泥板

狂亂

anaerobic

軍械庫(kù)

https://doi.org/10.1007/978-3-030-63982-2Limestone; Sedimentology; Stratigraphy; Diagensis; Geohistory

集聚成團(tuán)

陰險(xiǎn)

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 previou

Gustatory

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 silice

UTTER

Inferior

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

減至最低

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