南黄海千里岩附近海域第四纪构造活动特征

李官保; 刘保华; 赵月霞; 李炜; 姜丽丽

doi:10.3799/dqkx.2011.103

Volume 36 Issue 6

Jun. 2011

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Article Navigation > Earth Science > 2011 > 36(6): 977-984

LI Guan-bao, LIU Bao-hua, ZHAO Yue-xia, LI Wei, JIANG Li-li, 2011. Quaternary Tectonic Activity near the Qianliyan Island of Southern Yellow Sea. Earth Science, 36(6): 977-984. doi: 10.3799/dqkx.2011.103

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LI Guan-bao, LIU Bao-hua, ZHAO Yue-xia, LI Wei, JIANG Li-li, 2011. Quaternary Tectonic Activity near the Qianliyan Island of Southern Yellow Sea. Earth Science, 36(6): 977-984. doi: 10.3799/dqkx.2011.103

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Quaternary Tectonic Activity near the Qianliyan Island of Southern Yellow Sea

doi: 10.3799/dqkx.2011.103

LI Guan-bao^{1, 2
,},
LIU Bao-hua^{1, 2},
ZHAO Yue-xia^{1, 2},
LI Wei³,
JIANG Li-li³

1.
First Institute of Oceanography, SOA, Qingdao 266061, China
2.
Key Laboratory of Marine Sedimentary and Environmental Geology, SOA, Qingdao 266061, China
3.
Seismology Bureau of Qingdao, Qingdao 266071, China

Received Date: 2011-05-16
Available Online: 2021-11-10
Publish Date: 2011-06-15

Abstract

Abstract

Many Quaternary folds and faults are identified on the seismic reflection profiles acquired in the adjacent areas of Qianliyan Island of southern Yellow Sea. The faults are mainly of reverse fault. The folds are mainly gentle and tilted, caused by fault activities. Most folds and faults occurred below a plane of unconformity between middle Pleistocene and its overlying upper Pleistocene. Some faults, such as Qianliyan fault, are late Pleistocene active fault. Many faults and folds were synsedimentarily developed in the lower Pleistocene and underlying strata, revealling rather strong tectonic activity, especially at the basin boundary where the faults even cut into the late Pleistocene stratum. The formation of folds and faults was attributed to the last tectogenesis of the Yellow Sea in middle Pleistocene, which maybe correspond to the Kunlun-Huanghe movement of Qinghai-Tibet plateau. At that time, the N-S striking horizontal stress drove the early-developed basin boundary faults reactive and further induced the NEE or E-W striking tectonic deformation in the overlying sedimentary layer.
- southern Yellow Sea,
- Qianliyan Island,
- Quaternary,
- tectonic activity,
- tectogenesis,
- seismic profile

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References(63)

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Quaternary Tectonic Activity near the Qianliyan Island of Southern Yellow Sea

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