The high temperature abnormality area ( or belt ) of low frequency part of tirls is likely to attributed to the current tectonic activity and earthquake 低頻成份的高溫異常區(qū)(條帶)跟構造特征、地震活動密切相關。
Compared with weather data and earthquake activity , our result shows that thermal abnormality of low frequency part of tirls is resulted most possibly from fault activity and could offer a certain indictor for judging current tectonic activity or earthquake 結果表明,低頻成份的熱異常更接近于斷層活動所引起的熱信息,能為斷層或地震活動提供一定的指示信息。