Sitzungsberichte.

Indexes cataloged separately.

Sitzungberichte.

Vols. 43-64 issued in 2 series; v. 65-96 issued in 3 series: v. 97-131 issued in 4 series; v. 132- issued in 3 series: Abt. 1. Minerologie, Biologie, Erdkunde (varies); Abt. 2a. Mathematik, Astronomie, Physik, Meteorologie und Technik (varies slightly); Abt. 2b. Chemie.

Encyclopédie des sciences mathématiques pures et appliquées /

Issued in parts.

Sitzungsberichte /

Mode of access: Internet.

Fontes rerum Austriacarum.

Each issue also has a distinctive title.

Denkschriften /

GeoRef

Sitzungsberichte /

Imprint varies: Wien : Böhlaus, 1960-1972; Wien : Verlag der Österreichischen Akademie der Wissenschaften, 1973-<1988>

Nachrichten.

Number of issues per volume varies.

The Pico de Navas slump (Burgos, Spain): a large rocky landslide caused by underlying clayey sand fluidification

The Pico de Navas landslide was a large-magnitude rotational movement, affecting 50x106m3 of hard to soft rocks. The objectives of this study were: (1) to characterize the landslide in terms of geology, geomorphological features and geotechnical parameters; and (2) to obtain an adequate geomechanical model to comprehensively explain its rupture, considering topographic, hydro-geological and geomechanical conditions. The rupture surface crossed, from top to bottom: (a) more than 200 m of limestone and clay units of the Upper Cretaceous, affected by faults; and (b) the Albian unit of Utrillas facies composed of silty sand with clay (Kaolinite) of the Lower Cretaceous. This sand played an important role in the basal failure of the slide due to the influence of fine particles (silt and clay), which comprised on average more than 70% of the sand, and the high content presence of kaolinite (>40%) in some beds. Its geotechnical parameters are: unit weight (δ) = 19-23 KN/m3; friction angle (φ) = 13º-38º and cohesion (c) = 10-48 KN/m2. Its microstructure consists of accumulations of kaolinite crystals stuck to terrigenous grains, making clayey peds. We hypothesize that the presence of these aggregates was the internal cause of fluidification of this layer once wet. Besides the faulted structure of the massif, other conditioning factors of the movement were: the large load of the upper limestone layers; high water table levels; high water pore pressure; and the loss of strength due to wet conditions. The 3D simulation of the stability conditions concurs with our hypothesis. The landslide occurred in the Recent or Middle Holocene, certainly before at least 500 BC and possibly during a wet climate period. Today, it appears to be inactive. This study helps to understand the frequent slope instabilities all along the Iberian Range when facies Utrillas is present.

Leitungsgewalt und Kollegialität. Vom benediktinischen Beratungsrecht zum Konstitutionalismus deutscher Domkapitel und des Kardinalkollegs (ca. 500-1500).

Die kirchliche Verfassungsgeschichte des Mittelalters war von einer analogen Entwicklung scheinbar konträrer monarchischer und kollegialer Prinzipien geprägt. Dem Leitungsanspruch von Äbten, Bischöfen und Päpsten standen Beratungsrechte und Mitbestimmungsanliegen ihrer Mönche, Domkapitulare und Kardinäle gegenüber. Die Abhandlung zeigt auf, wie sich letztere im Verlauf der mittelalterlichen Geschichte als mehr oder weniger unabhängige Wahl- und Ratskollegien formierten und um eine Transformation eher unverbindlicher Beratungsfunktionen zu quasi parlamentarischen Rechten bemühten. Einschlägige verfassungsgeschichtliche Dokumente von der Benediktsregel aus dem 6. Jahrhundert bis hin zu bischöflichen und päpstlichen Wahlkapitulationen aus dem 15. Jahrhundert werden hinsichtlich ihrer kulturgeschichtlichen Zusammenhänge und Wirkungen analysiert.