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CONDUCTIVITY DISCONTINUITIES IN THE UPPER-MANTLE BENEATH A STABLE CRATON
Author(s): SCHULTZ A, KURTZ RD, CHAVE AD, JONES AG
Source: GEOPHYSICAL RESEARCH LETTERS    Volume: 20    Issue: 24    Pages: 2941-2944    Published: DEC 23 1993  
Times Cited: 75     References: 17     
Abstract: We present evidence for approximate collocation of seismic and electrical transitions in the upper mantle. More than two years of very long period magnetotelluric (MT) data were recorded at a lakebottom observatory in the central Canadian Shield. After processing to contend with non-stationary source effects, and removal of galvanic distortion, the underlying structure is ID for periods of one hour to four days. The response was extended to periods of 100 days by appending Geomagnetic Depth Sounding data to the MT curves. Minimum structure linearised inversion, nonlinear extremal inversion, and a new genetic algorithm for nonlinear hypothesis testing, reveal discrete jumps in conductivity at depths near the major upper mantle seismic discontinuities. The jumps occur over limited depth ranges.
Document Type: Article
Language: English
Reprint Address: SCHULTZ, A (reprint author), UNIV CAMBRIDGE, INST THEORET GEOPHYS, DEPT EARTH SCI, DOWNING ST, CAMBRIDGE CB2 3EQ, ENGLAND
Addresses:
1. GEOL SURVEY CANADA, OTTAWA K1A 0Y3, ON CANADA
2. WOODS HOLE OCEANOG INST, WOODS HOLE, MA 02543 USA
Publisher: AMER GEOPHYSICAL UNION, 2000 FLORIDA AVE NW, WASHINGTON, DC 20009
Subject Category: Geosciences, Multidisciplinary
IDS Number: MQ173
ISSN: 0094-8276
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