The development of gravity and magnetic studies, emphasizing articles published in the Geological Society of America Bulletin

1988 ◽  
Vol 100 (4) ◽  
pp. 469-478 ◽  
Author(s):  
G. R. KELLER
Geophysics ◽  
1943 ◽  
Vol 8 (4) ◽  
pp. 421-423
Author(s):  
L. L. Nettleton

This paper gives the geophysical results and interpretation for a rather close net of gravity and magnetic stations in the southern two‐thirds of New Jersey and eastern Pennsylvania. Over most of the New Jersey parts, the stations are at intervals of about 31/2 miles on profiles roughly ten miles apart, running approximately NW‐SE, or across the strike of the Appalachian trends. This work is supplemented by a zone of much closer control extending in a band about four miles wide reaching from Barnegat Bay on the coast, northwestward through Princeton and Flemington to the Delaware River at Phillipsburg, New Jersey.


2009 ◽  
Vol 51 (1) ◽  
Author(s):  
F. Cella ◽  
M. Fedi ◽  
G. Florio ◽  
V. Paoletti ◽  
A. Rapolla

2013 ◽  
Author(s):  
Jude King ◽  
C. M. Green ◽  
J. D. Fairhead ◽  
A. Salem ◽  
P. J. East

2020 ◽  
Vol 10 (10) ◽  
pp. 1009-1026
Author(s):  
Fosso Téguia M. Estelle Eric ◽  
Nana Gaelle Vanessa ◽  
Lepatio Tchieg Sterve Alain ◽  
Ntomb Biboum Edouard Olivier ◽  
Eyike Yomba Albert ◽  
...  

1994 ◽  
Vol 5 (4) ◽  
pp. 499 ◽  
Author(s):  
Chieh-Hou Yang ◽  
Tai-Chye Shei ◽  
Chung-Chia Lue

1990 ◽  
Vol 10 (1) ◽  
pp. 31-36 ◽  
Author(s):  
L. V. Subba Raju ◽  
K. A. Kamesh Raju ◽  
V. Subrahmanyam ◽  
D. Gopala Rao

Geophysics ◽  
1984 ◽  
Vol 49 (11) ◽  
pp. 2044-2047 ◽  
Author(s):  
Kenneth D. Mahrer ◽  
Chris Bradley ◽  
Sylvia Newsom

Gupta and Fitzpatrick (1971) remark that very little has been published on the correlation of topography and ground magnetic studies, specifically, magnetic‐terrain effects. Plouff (1976) discusses modeling of gravity and magnetic fields using polygonal prisms and the application to magnetic‐terrain anomalies. In both of these articles magnetic‐terrain anomalies from crystalline rocks are discussed. By contrast, this note discusses magnetic‐terrain anomalies identified in a ground magnetic survey within a sedimentary environment, specifically, across alluvial fans.


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