Mebus A. Geyh

Philipps University of Marburg

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Helmut Schleicher

Universität Hamburg

Martín Grosjean

Oeschger Centre for Climate Change Research

Blas L. Valero‐Garcés

Instituto Pirenaico de Ecología

Bruno Messerli

University of Bern

U. Schotterer

University of Bern

G. J. Hennig

Niedersächsisches Landesamt für Denkmalpflege

Bettina Jenny

Klinik und Poliklinik für Kinder- und Jugendpsychiatrie

Hans Schreier

University of British Columbia

Gert Michel

Geologischer Dienst Nordrhein-Westfalen (Germany)

Helmut Müller

Federal Institute for Geosciences and Natural Resources

Cooperative Institutions

Federal Institute for Geosciences and Natural Resources

University of Michigan–Ann Arbor

Geological Survey of Canada

University of Cambridge

University of Pennsylvania

University of Bern

Bridge University

Geological Survey of Finland

University of Saskatchewan

Niedersächsisches Landesamt für Denkmalpflege

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Absolute Age Determination

Springer eBooks (1990)

Mebus A. Geyh Helmut Schleicher

Absolute (philosophy)

10.1007/978-3-642-74826-4

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Citations (214)

Rezensionen

Zeitschrift für Geomorphologie (1981)

W. Andres Ian Douglas Barbara Gamper Martin Schwarzbach G. Stäblein

10.1127/zfg/25/1981/115

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Physical Dating Methods

Springer eBooks (1990)

Mebus A. Geyh Helmut Schleicher

Cosmogenic nuclide

Radiometric dating

Nuclide

10.1007/978-3-642-74826-4_5

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Citations (7)

RDC volume 4 Cover and Back matter

Radiocarbon (1962)

T. F. Dorn A. W. Fairhall William Schell Y. Takashima Milton Trautman

An abstract is not available for this content so a preview has been provided. As you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

10.1017/s0033822200036687

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10000 [i.e. Zehntausend] Jahre Gletschergeschichte der Erde

friedrich Röthlisberger Mebus A. Geyh

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Citations (2)

Einleitung

Springer eBooks (1983)

Mebus A. Geyh

10.1007/978-3-642-51148-6_1

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The application of the 14C and 3H methods for environmental studies by hydrology

Zeitschrift der Deutschen Geologischen Gesellschaft (1973)

Mebus A. Geyh

10.1127/zdgg/124/1973/515

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14C-Datierung limnischer Sedimente und die Eichung der14C-Zeitskala

The Science of Nature (1970)

Mebus A. Geyh Josef Merkt Helmut M�ller

10.1007/bf00598790

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Citations (8)

Rapport I.7. Reconstitutions paléo-climatiques et paléoécologiques à partir de l’étude des sédiments lacustres de l’Allemagne méridionale

Journées de l'hydraulique (1975)

Mebus A. Geyh Josef Merkt Heino Müller Hansjörg Streif

La partie inferieure des carottes du sediment lacustre des petits lacs de Schleinsee et Degersee pres du lac de Constance appartient au Tardiglacial et a l’Holocene jusqu’au sub-Boreal. Les coupes commencent par des varves lacustres-glaciaires qui sont suivies par des sediments sapropeliques deposes pendant une phase meromictique au Tardiglacial et a THolocene inferieur. Les sediments sus-jacents sont caracterises par une lamination saisonniere a calcaire. L’activite de l’homme se fait connaitre a partir des sediments contemporains de l’âge de Bronze.

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Origin of a fresh groundwater body in Cholistan, Thar Desert, Pakistan

Geological Society London Special Publications (2008)

Mebus A. Geyh D. Ploethner

Abstract The Thar Desert of Pakistan stretches along the border to India and is one of the most densely populated deserts in the world. Brackish to saline groundwater prevails. A locally restricted fresh groundwater resource was discovered by a comprehensive hydrogeological, geophysical, and isotope hydrological survey conducted from 1986 to 1991. The origin, recharge mechanism and age of the fresh groundwater resource were assessed. There is only fossil groundwater and this must be mined. Sodium is the predominant cation. Present groundwater recharge is absent or extremely low as the annual precipitation rate and the potential evapotranspiration rate amount to less than 200 mm/a and about 2700 mm/a, respectively. The investigations comprised a hydrogeological well inventory, electrical resistivity transects on the ground and an air-borne electromagnetic survey, followed by a test-hole drilling programme combined with geophysical borehole logging, aquifer testing, and groundwater sampling for both chemical and environmental isotope analyses. The results of this study delivered a hydrogeological concept on the origin and recharge of the fresh groundwater body. We found that the fresh groundwater was indirectly recharged during flash floods in low lands during the last pluvial period rather than directly replenished in the high mountain areas far in the east.

Desert (philosophy)

10.1144/sp288.8

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Citations (5)