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2022, 41(2) 373-385 DOI:
ISSN: 1004-5589 CN: 22-1111/P |
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Application of comprehensive geophysical prospecting in studying genetic mechanism of Changbai Dahu landslide in JilinProvinc |
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YUZerui1,2,3 ,FANGShi1,4 ,WANGYan2,3 ,DUJun5 ,CHENYang2,3 |
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１ＣｏｌｌｅｇｅｏｆＥａｒｔｈＳｃｉｅｎｃｅｓ，ＪｉｌｉｎＵｎｉｖｅｒｓｉｔｙ，Ｃｈａｎｇｃｈｕｎ１３００６１，Ｃｈｉｎａ；
２ＩｎｓｔｉｔｕｔｅｏｆＧｅｏｌｏｇｉｃａｌＭｉｎｅｒａｌＳｕｒｖｅｙａｎｄＤｅｓｉｇｎｏｆＪｉｌｉｎＰｒｏｖｉｎｃｅ，Ｃｈａｎｇｃｈｕｎ１３００１２，Ｃｈｉｎａ；
３ＧｅｏｌｏｇｙａｎｄＭｉｎｅｒａｌＣｏｎｓｔｒｕｃｔｉｏｎＧｒｏｕｐＣｏ，ＬｔｄｏｆＪｉｌｉｎＰｒｏｖｉｎｃｅ，Ｃｈａｎｇｃｈｕｎ１３００１２，Ｃｈｉｎａ；
４ＫｅｙＬａｂｏｒａｔｏｒｙｆｏｒＯｉｌＳｈａｌｅａｎｄＣｏｅｘｉｓｔｉｎｇＭｉｎｅｒａｌｓｏｆＪｉｌｉｎＵｎｉｖｅｒｓｉｔｙ，Ｃｈａｎｇｃｈｕｎ１３００６１，Ｃｈｉｎａ；
５ＬｉａｏｎｉｎｇＥｎｇｉｎｅｅｒｉｎｇＳｕｒｖｅｙａｎｄＤｅｓｉｇｎＩｎｓｔｉｔｕｔｅＣｏ，Ｌｔｄ，Ｊｉｎｚｈｏｕ１２１０００，Ｌｉａｏｎｉｎｇ，Ｃｈｉｎａ |
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Abstract：
ＴａｋｉｎｇｔｈｅＤａｈｕｌａｎｄｓｌｉｄｅｉｎＪｉｅｆａｎｇｖｉｌｌａｇｅ，ＣｈａｎｇｂａｉＫｏｒｅａｎＡｕｔｏｎｏｍｏｕｓＣｏｕｎｔｙ，ＪｉｌｉｎＰｒｏｖｉｎｃｅ ａｓａｎｅｘａｍｐｌｅ，ｔｈｅａｕｔｈｏｒｓｍａｋｅａｃｏｍｐｒｅｈｅｎｓｉｖｅｅｘｐｌｏｒａｔｉｏｎｗｉｔｈｔｈｅｈｅｌｐｏｆｈｉｇｈｄｅｎｓｉｔｙｅｌｅｃｔｒｉｃａｌｍｅｔｈｏｄａｎｄ ｍｕｌｔｉｃｈａｎｎｅｌｔｒａｎｓｉｅｎｔｓｕｒｆａｃｅｗａｖｅｍｅｔｈｏｄ．Ｔｈｉｓｃｏｍｂｉｎｅｄｗｉｔｈｔｈｅｄｒｉｌｌｉｎｇｒｅｓｕｌｔｓ，ｃｌａｒｉｆｉｅｓｔｈｅｓｈａｐｅ，ｍａｔｅｒｉａｌ ｃｏｍｐｏｓｉｔｉｏｎａｎｄｔｈｉｃｋｎｅｓｓｏｆｔｈｅｌａｎｄｓｌｉｄｅ，ｉｎｆｅｒｓｔｈｅｌｏｃａｔｉｏｎｏｆｔｈｅｓｌｉｄｉｎｇｓｕｒｆａｃｅ，ａｎｄａｎａｌｙｚｅｓｔｈｅｉｎｆｌｕｅｎｃｉｎｇ ｆａｃｔｏｒｓａｎｄｇｅｎｅｔｉｃｍｅｃｈａｎｉｓｍｏｆｔｈｅｌａｎｄｓｌｉｄｅ．ＴｈｅｒｅｓｕｌｔｓｓｈｏｗｔｈａｔｔｈｅＤａｈｕｌａｎｄｓｌｉｄｅｉｓａｆｆｅｃｔｅｄｂｙｌａｎｄｆｏｒｍ，ｌｉｔｈｏｌｏｇｙ，ｈｙｄｒｏｌｏｇｉｃａｌｃｏｎｄｉｔｉｏｎｓａｎｄｏｔｈｅｒｆａｃｔｏｒｓ．Ｄｕｅｔｏｍａｎｕａｌｅｘｃａｖａｔｉｏｎ，ｔｈｅｓｌｏｐｅｔｏｅｉｓｆｒｅｅａｎｄｔｅｎｓｉｏｎ ｃｒａｃｋｓａｒｅｆｏｒｍｅｄａｔｔｈｅｒｅａｒｅｄｇｅｏｆｔｈｅｓｌｏｐｅ．Ｒａｉｎｆａｌｌｉｎｆｉｌｔｒａｔｉｏｎｒｅｄｕｃｅｓｔｈｅｓｈｅａｒｓｔｒｅｎｇｔｈｏｆｒｏｃｋａｎｄｓｏｉｌ ｍａｓｓ，ｒｅｓｕｌｔｉｎｇｉｎｃｒｅｅｐｄｅｆｏｒｍａｔｉｏｎａｌｏｎｇｔｈｅｆｏｕｎｄａｔｉｏｎｏｖｅｒｂｕｒｄｅｎｉｎｔｅｒｆａｃｅ（ｓｌｉｄｉｎｇｓｕｒｆａｃｅ）．Ｗｉｔｈｔｈｅａｃｃｕｍｕｌａｔｉｏｎｏｆｓｌｏｐｅｓｔｒｅｓｓ，ｔｈｅｄｅｆｏｒｍａｔｉｏｎｉｎｔｅｎｓｉｆｉｅｓ，ａｎｄｆｉｎａｌｌｙｌｅａｄｓｔｏｓｌｏｐｅｉｎｓｔａｂｉｌｉｔｙａｎｄｆａｉｌｕｒｅ．ＴｈｅｇｅｏｍｅｃｈａｎｉｃａｌｍｏｄｅｌｏｆｔｈｅＤａｈｕｌａｎｄｓｌｉｄｅｉｓｃｒｅｅｐｔｅｎｓｉｏｎｃｒａｃｋ，ａｎｄｉｔｓｅｖｏｌｕｔｉｏｎｐｒｏｃｅｓｓｅｓｃａｎｂｅｓｕｍｍａｒｉｚｅｄｉｎｔｏｔｈｒｅｅ ｓｔａｇｅｓ：ｌａｎｄｓｌｉｄｅｃｒｅｅｐｄｅｆｏｒｍａｔｉｏｎ，ｓｌｏｐｅｃｒａｃｋｄｅｖｅｌｏｐｍｅｎｔａｎｄｌａｎｄｓｌｉｄｅｓｌｉｄｉｎｇｉｎｓｔａｂｉｌｉｔｙ |
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Keywords：
ｌａｎｄｓｌｉｄｅ
ｈｉｇｈｄｅｎｓｉｔｙｅｌｅｃｔｒｉｃａｌｍｅｔｈｏｄ
ｔｒａｎｓｉｅｎｔｓｕｒｆａｃｅｗａｖｅｍｅｔｈｏｄ
ｇｅｎｅｔｉｃｍｅｃｈａｎｉｓｍ
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