scholarly journals Geoelectric and electromagnetic measurements within an organized archaeological framework: the Marzabotto example

1994 ◽  
Vol 37 (5 Sup.) ◽  
Author(s):  
E. Bozzo ◽  
S. Lombardo ◽  
F. Merlanti ◽  
M. Pavan

Geophysical prospecting was Performed in the Etruscan settlement of Marzabotto, near Bologna (Italy), to find shallow anthropic structures within an almost homogeneous environment. This paper describes some results of the geoelectric and electromagnetic VLF methods used. Non-standard geoelectric devices, such as the tripotential, twin-probe and the Offset-Wermer methods, were applied. The set of results was compared to classical dipolar sections. The Offset-Wenner device was useful for detecting vertically striking structures. Conversely, the electromagnetic VLF techniques are not suitable for investigating structures with a negligible contrast of conductivity with the environment. Prospecting data generated a general pattern of anomalies and some were confirmed by excavation samples, showing walIs, floors, water wells and other remains of urban structures.

Geophysics ◽  
1955 ◽  
Vol 20 (4) ◽  
pp. 886-912 ◽  
Author(s):  
J. F. Enslin

The major application of geophysical prospecting in the Union of South Africa is in determining locations for drilling water wells. Four principal approaches are employed: 1. Permeable contact zones between igneous intrusions and sedimentary rocks are sought by magnetic surveys. 2. Basins of decomposition are sought by the resistivity method. 3. Narrow water‐bearing fissures and fault zones are located by an electromagnetic method. 4. The water‐bearing and water‐yielding properties of rocks are determined from their computed resistivities. The interpretation of resistivity depth probe curves is based on an empirical method which corrects for lateral effects. Another important application of geophysical prospecting in the Union is in gold‐mining. Gravitational and magnetic surveys have been widely used in the search for auriferous reefs in the Wit‐waterstand system which are concealed by a deep cover of younger rocks. Resistivity, electromagnetic, gravitational, and seismic methods have been applied to problems of engineering geology, including the delineation of areas in dolomite where sinkholes may occur.


1928 ◽  
Vol 138 (5) ◽  
pp. 414-417 ◽  
Author(s):  
A. S. Eve ◽  
D. A. Keys

Waterlines ◽  
1988 ◽  
Vol 6 (4) ◽  
pp. 10-13
Author(s):  
Alan Hayes
Keyword(s):  

1937 ◽  
Author(s):  
E.A. Sergeev ◽  
A.P. Solovov ◽  
H. E. Hawkes

1995 ◽  
Author(s):  
J.I. Steiger ◽  
Richard Kessler
Keyword(s):  

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