
Heat Flow at Broken Hill, New South Wales
Author(s) -
Sass J. H.,
Marne A. E. Le
Publication year - 1963
Publication title -
geophysical journal of the royal astronomical society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.302
H-Index - 168
eISSN - 1365-246X
pISSN - 0016-8009
DOI - 10.1111/j.1365-246x.1963.tb07090.x
Subject(s) - heat flow , geology , thermal conductivity , drill , heat flux , drill hole , square (algebra) , flow (mathematics) , high heat , thermal , heat transfer , mineralogy , petrology , geomorphology , mechanics , meteorology , materials science , geometry , composite material , mathematics , geography , metallurgy , physics
Summary The heat flow in the Broken Hill region has been determined from temperatures measured in 18 deep depressed drill holes covering an area of 200 square miles and in 32 horizontal drill holes in mine walls. 118 thermal conductivity determinations on rock specimens representative of the area have been used. The values of heat flux range from 1.81 to 2.07 μcal/cm 2 s with a mean of 1.93. The standard error of a single determination is about 5 per cent.