Thomas,St.: Beitrag zur Protein- und Biogaserzeugung aus hochbelasteten Abwässern. Gewässerschutz — Wasser — Abwasser 107, Aachen,Ges. z. Förder. d Siedlungswasserwirtsch. an d. RWTH Aachen e. V., 1981, 171 S., 8 Anl., 63 Abb., 29 Tab., DM 40,—, ISSN 0342–6068     

H.-J. Walther 《洁净——土壤、空气、水》1990,18(1):152-152

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Über die Sedimente der Flachsee im Lothringer Jura     

Dr. Walther Klüpfel 《International Journal of Earth Sciences》1916,7(3-4):97-109

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Über die Form andiner Krustenbewegungen und ihre Beziehungen zur Sedimentation     

Professor Walther Penck 《International Journal of Earth Sciences》1924,14(3):301-315

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Die alten Gebirge der Provinz Buenos Aires     

Walther Schiller 《International Journal of Earth Sciences》1933,24(3-4):220-221

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Das Faziesgesetz der vorquartären Vulkaneruptionen     

Walther Klüpfel 《International Journal of Earth Sciences》1933,24(1-2):28-56

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Burdigal- und Helvettransgression im Rheintalgraben     

Walther Klüpfel 《International Journal of Earth Sciences》1931,22(3-4):179-186

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Facies architecture and sedimentology of a meandering fluvial system: a Palaeogene example from the Weisselster Basin, Germany   总被引：1，自引：0，他引：1  

Jochen Halfar  Walter Riegel  & Harald Walther 《Sedimentology》1998,45(1):1-17

The Schleenhain open pit coal mine, located 30 km south of Leipzig, Germany, exposes Upper Eocene and Oligocene non-marine strata representing fluvial deposition in the centre of the Weisselster Basin. Active mining and successive cuts provided the rare opportunity to obtain a three-dimensional perspective of laterally extensive surface outcrops. These were used to construct a detailed fence diagram, which provided the basis for recognition of key architectural elements in the weakly consolidated meandering stream deposits. In addition to the eight basic architectural elements of Miall (1985 ), the element SL (shallow lake deposits) was newly defined and the element CH (channel) was subdivided into CHg (palaeo-river system) and CHk (small channel). The profiles contain parts of two fining-upward cycles, which are separated by an unconformity spanning the Early Oligocene. Deposits of the first cycle begin with transverse sand bars (downstream accretion deposits-DA) and point bars (lateral accretion deposits-LA). The upper part of the cycle is represented by overbank fines (OF) and the element SL, which consists of laterally discontinuous lenses of dark, plant-bearing, kaolinite-rich clays, that were deposited in shallow lakes adjacent to the active channel. Coal seams interlayered with palaeosols are the main constituents of element OF. Sheetlike bodies of medium to fine gravels (gravel bars and bedforms-GB) on an erosive coal surface mark the beginning of the second cycle. Dissolution of underlying Permian salts and sulphates prior to, during, and after the deposition of the Palaeogene strata caused the development of two synclines within the outcrop. Coal seams and clay horizons which thicken and dip towards the centre of the synclines, provide evidence for their chronological development.  相似文献   

Twentieth-century trends in the thermal growing season in the Greater Baltic Area   总被引：4，自引：0，他引：4  

Hans W. Linderholm  Alexander Walther  Deliang Chen 《Climatic change》2008,87(3-4):405-419

Phenological data have shown an increase of ca. 10 days in European growing season length in the latter part of the twentieth century. In general, these changes have been associated with global warming. Here we present a study of thermal growing season (GS) trends in the Greater Baltic Area, northern Europe. Yearly dates for the start, end and length of the GS were computed for 49 stations in the studied area, using daily mean temperature measurements. Trends and tendencies of the GS parameters were analysed within the twentieth century. We also examined GS trends in long records (starting before 1850) from the region. The results show a general increase of the length of the GS of ca one week since 1951 in the area, where the most considerable change has occurred in spring (starting ∼6 days earlier). The largest increases were found at stations adjacent to the Baltic Sea and North Sea, where some Danish stations showed significant increasing trends in the length of the GS of more than 20 days. The only tendency for a shorter GS was found in Archangelsk, north western Russia. The three longest records displayed large inter-annual and decadal variability, with tendencies for increased frequencies of longer growing seasons since the 1950s.  相似文献   

Zur Kenntnis des Lothringer Bathonien     

Klüpfel  Walther 《International Journal of Earth Sciences》1916,7(1-2):1-29

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Die Alpin-Mediterrane Metallogenese     

Prof. Dr. Walther E. Petrascheck 《International Journal of Earth Sciences》1964,53(1):376-389

Zusammenfassung Die ostmediterrane Erzprovinz, die Kleinasien und die Balkanhalbinsel umfaßt, ist gekennzeichnet durch die enge Bindung ihrer Lagerstätten an die sehr zahlreichen sichtbaren Zentren des alpidischen Magmatismus. In der karpatisch-alpinen Erzprovinz sind die Lagerstätten räumlich, zeitlich und stofflich mit der alpinen Kristallisationsmetamorphose verknüpft. Sie finden sich häufig an Überschiebungsflächen und ihre vorwiegende Form ist die der metasomatischen Lager. In der westmediterranen Erzprovinz, vor allem im Atlas-Gebirge, treten die Lagerstätten an steilen Brüchen und z. T. auch in flachen, selektiv verdrängten oder imprägnierten Schichten auf. Trotz dieser Unterschiede, die durch das regionale geologische Milieu erklärt werden können, zeigen die drei alpin mediterranen Erzprovinzen wichtige Gemeinsamkeiten: gleiches Alter wie der alpine Magmatismus in der ganzen Kette, Vorherrschen der Metalle Cu, Au, Fe (als Siderit) im Nordstamm und der Metalle Pb, Zn, Sb, Cr im Südstamm des Orogens und die Abwesenheit bzw. das Zurücktreten von Co, Ni, U, Sn. Die Vererzungsdichte in den drei Provinzen ist ähnlich, die Lagerstättenformen sind verschieden.

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The Eastern Mediterranean ore province covering Asia and the Balkan-countries is characterized by a direct relation of its deposits to the mostly visible centres of the alpine magmatism. In the Alpine-Carpathian province the deposits are related to the Alpine metamorphism by distribution, age and substantial composition. They frequently occur along overthrust planes and many of them are replacement bodies. The deposits in the Western-Mediterranean province, especially in the Atlas Mountains, are to be found in steep faults- and partially in flat layers being impregnated and selectivity replaced. In spite of such differences which can be understood by the regional geological environment, the three Alpine-Mediterranean metallogenetic provinces show some important common features: they are contemporaneous with the alpine magmatism in the whole belt and Cu, Au, Fe (siderite) predominate in the northern wing, while Pb, Zn, Sb, Cr do so in the southern wing. Co, Ni, U, Sn, are nearly absent. The intensity of the mineralisation in the three provinces is similar whereas the forms of the deposits are different.

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Résumé La province métallogenique de la Mediterranée Orientale qui comprend l'Anatolie et la Peninsule Balkanique, est characterisée par un rapport étroit de ses gisements avec les nombreuses centres d'un magmatisme visible. Dans la province Carpatho-alpine les gisements sont liés par space, par âge et par substance avec le métamorphisme alpin. Ils se trouvent souvent dans les surfaces de charriage et leur forme prépondérante est celle des amas de substitution. Dans la province occidentale, surtout dans la chaine de l'Atlas, les gisements apparaissent dans des failles verticales et aussi dans des couches horizontales, formées par imprégnation et substitution sélective. Malgrès ces differences, qui sont explicables par le milieu géologique regional, les trois provinces métallogeniques ont des traits communs essentiels: Contemporainité avec le magmatisme alpin dans toute la chaine, préponderance de Cu, Au, siderose dans le rameau septentrional du système orogenique, préponderance du Pb, Zn, Sb et Cr dans le rameau méridional et l'absence quasi-totale du Co, Ni, U, Sn. L'intensité de la mineralisation dans les trois provinces se resemble, mais les formes des gisements sont differents.

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