scholarly journals Crustal structure at Nanga Parbat, northern Pakistan, from magnetotelluric soundings

1997 ◽  
Vol 24 (19) ◽  
pp. 2415-2418 ◽  
Author(s):  
Stephen K. Park ◽  
Randall J. Mackie
Keyword(s):  
Crustal Structure ◽  
Northern Pakistan ◽  
Magnetotelluric Soundings ◽  
Nanga Parbat

Tectonic exhumation of the Nanga Parbat massif, northern Pakistan

1995 ◽  
Vol 133 (1-2) ◽  
pp. 213-225 ◽  
Author(s):  
Mary S. Hubbard ◽  
David A. Spencer ◽  
David P. West
Keyword(s):  
Northern Pakistan ◽  
Nanga Parbat ◽  
Tectonic Exhumation

Exhumation overrated at Nanga Parbat, northern Pakistan

1996 ◽  
Vol 260 (1-3) ◽  
pp. 215-226 ◽  
Author(s):  
Alan G. Whittington
Keyword(s):  
Northern Pakistan ◽  
Nanga Parbat

Crustal structure of an intraplate thrust belt: The Iberian Chain revealed by wide-angle seismic, magnetotelluric soundings and gravity data

2015 ◽  
Vol 663 ◽  
pp. 339-353 ◽  
Author(s):  
Hoël Seillé ◽  
Ramon Salas ◽  
Jaume Pous ◽  
Joan Guimerà ◽  
Josep Gallart ◽  
...  
Keyword(s):  
Crustal Structure ◽  
Gravity Data ◽  
Wide Angle ◽  
Thrust Belt ◽  
Magnetotelluric Soundings ◽  
Iberian Chain

Resistive (dry?) lower crust in an active orogen, Nanga Parbat, northern Pakistan

2000 ◽  
Vol 316 (3-4) ◽  
pp. 359-380 ◽  
Author(s):  
Stephen K. Park ◽  
Randall L. Mackie
Keyword(s):  
Lower Crust ◽  
Northern Pakistan ◽  
Nanga Parbat

scholarly journals Crustal structure of the Gulf of Corinth in Central Greece, determined from magnetotelluric soundings

1997 ◽  
Vol 40 (1) ◽  
Author(s):  
G. Chouliaras ◽  
V. N. Pham ◽  
D. Boyer ◽  
P. Bernard ◽  
G. N. Stavrakakis
Keyword(s):  
Electrical Properties ◽  
Crustal Structure ◽  
Upper Mantle ◽  
Magnetotelluric Sounding ◽  
Crust And Upper Mantle ◽  
Magnetotelluric Soundings ◽  
Central Greece ◽  
Gulf Of Corinth ◽  
Conductive Zone ◽  
Epicentral Region

The magnetotelluric sounding method at 15 sites was employed to investigate the electrical properties of the crust and upper mantle near the epicentral region of the June 15 1995, Ms = 6.1, destructive earthquake in the Gulf of Corinth, Central Greece. The magnetotelluric results indicate the presence of a conductive zone in the mid-crust at a depth of 9 to 12 km near the seismogenetic region. The existence of this zone with a thickness of around 7 km can be explained by the presence of fluids in a zone of ductile shear. A second electrical discontinuity was also found at a depth of about 28 km and this may well correspond to the Moho below the Gulf of Corinth.

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