By Karl B. Föllmi

ISBN-10: 0387513590

ISBN-13: 9780387513591

This edited quantity includes sixteen learn articles. It offers fresh and urgent matters in stochastic approaches, keep watch over conception, differential video games, optimization, and their functions in finance, production, queueing networks, and weather keep an eye on. one of many salient gains is that the booklet is very multi-disciplinary. The publication is devoted to Professor Suresh Sethi at the party of his sixtieth birthday, in view of his distinctive profession.

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Extra resources for Evolution of the mid-Cretaceous triad: platform carbonates, phosphatic sediments, and pelagic carbonates along the northern Tethys margin

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Wannenalp Bed. Weathered surface of a multi-event winnowed and condensed phosphatic bed. The phosphatized particles consist of fossil debris (ammonoids: b___hb= Beudanticeras beudanti (BRONGNIART); h__o= Hysteroceras cf. ; inoceramids: bc = Birostrina concentrica (PARKINSON); bs = Birostrina sulcata (PARKINSON); sponges = s; solitary corals = c__), which are embedded in a sandy Hedbergella micrite Phosphates of the Plattenwald Bed appear as: A. Densely packed phosphatized fossil debris and lithoclasts, embedded in nonphosphatized sediments.

The outer shelf part is underlain by the Lower to lower Upper Aptian Mittagspitz Formation (Sect. 2) and overlain by the uppermost Aptian and A1bian Rankweil Beds and Freschen Beds (Sects. 2), which similarly suggests a middle late Aptian age. The middle Upper Aptian detritus-rich depositional system tract probably developed within 1 my. 1 General Overview In latest Aptian time (jacobi Zone), the deposition of predominantly detritusrich, clastic sediments ended, and a regime of retarded sediment accumulation took over, dominated by major episodes of erosion and redeposition (Figs.

2; sections 2, 3 in Fig. 29; Fig. 30). In the intermediate inner shelf, south of the Kamm Bed distribution area, the oldest Seewen sediments, on top of the Aubrig Beds, date from the brotzeni Zone (early Cenomanian) and sediments with an appenninica Zone age are confined to the uppermost Aubrig Beds and to a thin transitional sequence between the Aubrig Beds and the Seewen Formation. In distal inner shelf areas, the oldest Seewen sediments, on top of the Plattenwald Bed, commonly display an uppermost Albian age (appenninica Zone).

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Evolution of the mid-Cretaceous triad: platform carbonates, phosphatic sediments, and pelagic carbonates along the northern Tethys margin by Karl B. Föllmi


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