Relationship between electrical and thermal conductivities for evaluating thermal regime of gas hydrate bearing sedimentary layers

Annals of the New York Academy of Sciences

Volumn 912, Issue , 2000, Pages 167-172

  Matsubayashi, Osamu ^a   Edwards, R Nigel ^b  

^a GEOLOGICAL SURVEY OF JAPAN   (Japan)

^b UNIVERSITY OF TORONTO   (Canada)

Author keywords

[No Author keywords available]

Indexed keywords

CONFERENCE PAPER; ELECTRIC CONDUCTIVITY; MODEL; SEDIMENT; THERMAL CONDUCTIVITY;

EID: 0033925545     PISSN: 00778923     EISSN: None     Source Type: Book Series    
DOI: 10.1111/j.1749-6632.2000.tb06770.x     Document Type: Conference Paper

References (5)

1. 1. YAMANO, M. et al. 1982. Estimates of heat flow derived from gas hydrates. Geology 10: 339-343.
2. 2. MATSUBAYASHI, O. 1998. Heat flow measurement as an exploration tool for subbottom methane hydrates. Bull. Geol. Surv. Japan 49: 541-549.
3. 3. RUPPEL, C. 1998. Anomalously cold temperatures observed at the base of the gas hydrate stability zone on the U.S. Atlantic passive margin. Geology 25: 699-702.
4. 4. WOODSIDE, W. & J.H. MESSMER. 1961. Thermal conductivity of porous media. J. Appl. Phys. 32: 1688-1706.
5. 5. EDWARDS, R.N. 1997. On the resource evaluation of marine gas hydrate deposits using sea-floor transient electric dipole-dipole methods. Geophys. 62: 63-74.