中山大学学报(自然科学版)
中山大學學報(自然科學版)
중산대학학보(자연과학판)
ACTA SCIENTIARUM NATURALIUM UNIVERSITATIS SUNYATSENI
2014年
6期
37-44
,共8页
毕丽思%何宏林%徐岳仁%魏占玉%石峰%孙浩越
畢麗思%何宏林%徐嶽仁%魏佔玉%石峰%孫浩越
필려사%하굉림%서악인%위점옥%석봉%손호월
冲沟纵剖面%数学拟合函数%DEM数据%霍山山前断裂带%构造响应
遲溝縱剖麵%數學擬閤函數%DEM數據%霍山山前斷裂帶%構造響應
충구종부면%수학의합함수%DEM수거%곽산산전단렬대%구조향응
longitudinal profiles of the gullies%mathematical fitting functions%DEM data%the Huoshan piedmont fault%responses to the tectonic movement
处于不同构造环境以及不同发育阶段的冲沟会呈现出不同的数学函数形态特征,常见的有线性函数、指数函数、对数函数以及乘幂函数等。它们反映了冲沟演化对发育时间、区域气候特征、河床基岩性质和构造运动等因素的响应。基于DEM数据提取了横跨霍山山前断裂带的64条冲沟,分析了冲沟纵剖面的拟合函数及其所反映的冲沟对断裂活动的响应特征。结果显示,横跨霍山山前断裂带的冲沟均表现为幼年期的线性函数形态或轻微下凹的指数函数形态,这反映了上新世以来霍山山前断裂带持续而强烈的正断层作用,尤其是全新世以来时间间隔较短的多次强烈活动。
處于不同構造環境以及不同髮育階段的遲溝會呈現齣不同的數學函數形態特徵,常見的有線性函數、指數函數、對數函數以及乘冪函數等。它們反映瞭遲溝縯化對髮育時間、區域氣候特徵、河床基巖性質和構造運動等因素的響應。基于DEM數據提取瞭橫跨霍山山前斷裂帶的64條遲溝,分析瞭遲溝縱剖麵的擬閤函數及其所反映的遲溝對斷裂活動的響應特徵。結果顯示,橫跨霍山山前斷裂帶的遲溝均錶現為幼年期的線性函數形態或輕微下凹的指數函數形態,這反映瞭上新世以來霍山山前斷裂帶持續而彊烈的正斷層作用,尤其是全新世以來時間間隔較短的多次彊烈活動。
처우불동구조배경이급불동발육계단적충구회정현출불동적수학함수형태특정,상견적유선성함수、지수함수、대수함수이급승멱함수등。타문반영료충구연화대발육시간、구역기후특정、하상기암성질화구조운동등인소적향응。기우DEM수거제취료횡과곽산산전단렬대적64조충구,분석료충구종부면적의합함수급기소반영적충구대단렬활동적향응특정。결과현시,횡과곽산산전단렬대적충구균표현위유년기적선성함수형태혹경미하요적지수함수형태,저반영료상신세이래곽산산전단렬대지속이강렬적정단층작용,우기시전신세이래시간간격교단적다차강렬활동。
Longitudinal profiles of the gullies in different tectonic settings and different evolutionary sta-ges show different morphological forms which can be fitted ordinarily by such mathematical functions as linear function,exponential function,logarithmic function and power function.These forms reflect the re-sponse of the gullies to the factors such as the time,the climate,the bedrock of the riverbed and the tec-tonic movement.Based on DEM data,64 gullies across the Huoshan piedmont fault are extracted and their profiles are fitted by four types of mathematical functions above.The best-fitting mathematical func-tion for each gully is selected and the responding characteristics of the gullies to the tectonic movement of the fault are analyzed.The result shows that the gullies are in their infancy which is exhibited by their linear forms or the exponential forms with very small concavity.This is due to the response of the gullies to the constant normal-fault movement of the Huoshan piedmont fault since Pliocene, especially the strong activities with short interval in Holocene.