长白山玄武岩区地热异常区遥感识别

doi:10.13278/j.cnki.jjuese.201706205

Abstract

Abstract: The surface temperature of Changbai Mountain basalt area was interpreted by using Landsat TM5 multispectral and infrared data, and the potential geothermal fields were identified by using discrimination analysis on the surface temperature, hot springs and geothermal well distribution, gravity, and magnetic fields. The results show that the surface temperature abnormal areas are mainly distributed around the Tianchi volcano area on Changbai Mountain and the three Mesozoic sedimentary basins (Fusong, Songjiang, and Changbai basins). The proportion of abnormal pixel in surface temperature is 2.993%. The potential geothermal fields in the study area are divided into four regions, including the area around Changbai Mountain Tianchi volcano, Songjianghe-Fusong County, Erdaobaihe-Songjiang Country (Fusong and Songjiang basins), and Xianrenqiao-Changbai County-Shisidaogou(Changbai basin). The probability of potential geothermal resources is greater than 0.9, and the maximum value is 1.0 in Changbai Mountain Tianchi volcano region. The study provides a new approach for potential geothermal field identification.

Key words: potential geothermal filed, remote sensing identification, discrimination analysis method, Changbai Mountain basalt area

CLC Number:

P314.1

Yan Baizhong, Qiu Shuwei, Xiao Changlai, Liang Xiujuan. Potential Geothermal Fields Remote Sensing Identification in Changbai Mountain Basalt Area[J].Journal of Jilin University(Earth Science Edition), 2017, 47(6): 1819-1828.

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Potential Geothermal Fields Remote Sensing Identification in Changbai Mountain Basalt Area

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