Cooling of an igneous dike 20 yr after intrusion

Geology

Volumn 25, Issue 8, 1997, Pages 711-714

  Connor, C B ^a  

^a SOUTHWEST RESEARCH INSTITUTE   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

CONDENSATION; COOLING; HEAT FLUX; LEVEES; THERMODYNAMIC PROPERTIES;

FIELD OBSERVATIONS; HIGH TEMPERATURE; LOW RESISTIVITY; MEASURED TEMPERATURES; NONISOTHERMAL FLOWS; STEAMING GROUNDS; THERMAL ANOMALIES; UNSATURATED ZONE; ANALYTIC MODELS;

HYDRAULIC STRUCTURES;

CINDER CONE; COOLING; DEFORMATION MECHANISM; DIKE; HEAT FLOW; IGNEOUS INTRUSION; IGNEOUS ROCK; TEMPERATURE ANOMALY; TWO PHASE FLOW; VOLCANIC ERUPTION; DYKE; INTRUSION; THERMOPHYSICAL PROPERTIES;

KAMCHATKA; RUSSIAN FEDERATION; TOLBACHIK VOLCANO; TOLBACHIK;

EID: 0031452112     PISSN: 00917613     EISSN: None     Source Type: Journal    
DOI: 10.1130/0091-7613(1997)025<0711:COAIDY>2.3.CO;2     Document Type: Article

References (2)

1. Bailsford, A. D., and Major, K. G., 1964, The thermal conductivity of aggregates of several phases, including porous materials: British Journal of Applied Physics, v. 15, p. 313-319.
2. Buscheck, T. A., and Nitao, J. J., 1993, The analysis of repository-heat-driven hydrothermal flow at Yucca Mountain, in Proceedings, Site Characterization and Model Validation, Focus '93: LaGrange Park, Illinois, American Nuclear Society, p. 127-144.