Heat-flow distribution in Southeast Asia with consideration of volcanic heat

被引:20
作者
Nagao, T
Uyeda, S
机构
[1] TEXAS A&M UNIV,DEPT GEOPHYS,COLLEGE STN,TX 77843
[2] TEXAS A&M UNIV,GEODYNAM RES INST,COLLEGE STN,TX 77843
[3] TOKAI UNIV,SCH MARINE SCI & TECHNOL,SHIMIZU,SHIZUOKA 424,JAPAN
关键词
D O I
10.1016/0040-1951(95)00084-4
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
As of 1995, in Southeast Asia, from 15 degrees S to 25 degrees N and from 90 to 160 degrees E, 2539 heat flow measurements are available. Despite a recent increase in the number of measurements, still important data gaps exist in the region, especially around the volcanic regions. So far the contribution of heat flux from active volcanoes has largely been overlooked in regional heat-flow maps because of uncertainties surrounding it. We have tried to estimate the volcanic heat in this region with the assumption that these volcanoes emit a similar amount of heat as those in northeast Honshu, Japan, where heat-flow studies and seismic tomography enable us to estimate that, as a first approximation, a volcano can be represented by 140 mW/m(2) of heat flow. A heat-flow map including volcanic heat estimated in this way, makes the heat flow in the Sunda Are and the Philippines, where conventional heat-flow data are scarce, much higher than on a map without the volcanic heat.
引用
收藏
页码:153 / 159
页数:7
相关论文
共 28 条
  • [11] ANALYSIS OF VARIATION OF OCEAN-FLOOR BATHYMETRY AND HEAT-FLOW WITH AGE
    PARSONS, B
    SCLATER, JG
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH, 1977, 82 (05): : 803 - 827
  • [12] PUSPITO T, 1993, TECTONOPHYSICS, V230, P175
  • [13] Simkin T., 1981, VOLCANOES WORLD
  • [14] TAPPONNIER P, 1982, GEOLOGY, V10, P611, DOI 10.1130/0091-7613(1982)10<611:PETIAN>2.0.CO
  • [15] 2
  • [16] Taylor B., 1983, AGU MONOGRAPH, V27, P23, DOI DOI 10.1029/GM027P0023
  • [18] THIENPRASERT A, 1984, TECTONOPHYSICS, V121, P45
  • [19] THIENPRASERT A, 1978, UN ESCAP CCOP TECHN, V12, P17
  • [20] Uyeda S., 1980, UESCAP CCOP SOPAC TE, V3, P153