By Karl B. Föllmi
ISBN-10: 0387513590
ISBN-13: 9780387513591
This edited quantity includes sixteen study articles. It offers contemporary and urgent concerns in stochastic methods, keep watch over idea, differential video games, optimization, and their functions in finance, production, queueing networks, and weather regulate. one of many salient beneficial properties is that the ebook is extremely multi-disciplinary. The publication is devoted to Professor Suresh Sethi at the get together of his sixtieth birthday, in view of his uncommon profession.
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Additional info for Evolution of the mid-Cretaceous triad: platform carbonates, phosphatic sediments, and pelagic carbonates along the northern Tethys margin
Sample text
B. Slabbed specimen (phase 3 and 4 in Fig. 17). ) in the Plattenwald Bed, superjacent to Klaus Beds, indicate the jacobi and the early tardefurcata Zones as the time range in which this depositional sequence developed. This age is consistent with the biostratigraphic results obtained from east Swiss Tw~riberg Bed localities (presence of I4ypacanthoplites and Leymeriella; Ganz 1912; FOllmi and Ouwehand 1987). 1 General Overview Albian sediments of the Vorarlberg inner shelf reflect an episode of extensive phosphatization and condensation.
Outcrops in the area of the "Hohe Kuger' (in a small, klippen-like nappe remnant of probably ultrahelvetic origin; Fig. 1; Oberhauser 1953, 1958, 1982; F611mi 1986) display sediments of the Garschella and Seewen Formations in a facies characteristic of distal outer shelf regions. The lower sequence of the Freschen Beds is replaced by an alternation of spiculitic, radiolarian, and Hedbergella-bearing micrites and pseudosparites (comparable to calcareous beds in Brisi Beds, facies type D, and in Gams Beds), and dark, laminated, Freschen Beds-like marls and clays (Upper Aptian Hoehkugel Beds; max.
The interchannel areas are characterized by persistent low sediment accumulation rates (during latest Aptian to earliest Turonian) and by extensive phosphatization, which resulted in the formation of autochthonous and condensed phosphates (during latest Aptian to earliest Albian; section 2 in Fig. 15; Figs. 16 and 19; Plattenwald Bed; Sect. 1). 5. In outer shelf areas, sedimentation of the lower sequence of the Freschen Beds continued. , section 12 in Fig. 7). These beds depict distal offshoots of the Rankweil Beds (Fig.
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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