Quaternary activity characteristics of the Qionghua–Liantang fault belt in Hainan

YANG Xiaoxiao; HU Daogong; JIA Liyun; WANG Chaoqun; SUN Dongxia; ZHANG Lei

doi:10.12090/j.issn.1006-6616.2022020

Volume 29 Issue 1

Feb. 2023

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Article Navigation > Journal of Geomechanics > 2023 > 29(1): 127-137

YANG X X，HU D G，JIA L Y，et al.，2023. Quaternary activity characteristics of the Qionghua–Liantang fault belt in Hainan[J]. Journal of Geomechanics，29（1）：127−137 doi: 10.12090/j.issn.1006-6616.2022020

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Quaternary activity characteristics of the Qionghua–Liantang fault belt in Hainan

doi: 10.12090/j.issn.1006-6616.2022020

YANG Xiaoxiao^{1, 2, 3
,},
HU Daogong^{1, 2, 3
,
,},
JIA Liyun^{1, 2, 3},
WANG Chaoqun^{1, 2, 3},
SUN Dongxia^{1, 2, 3},
ZHANG Lei^{1, 2, 3}

1.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
2.
Key Laboratory of Active Tectonics and Geological Safety, Ministry of Natural Resources, Beijing 100081, China
3.
Research Center of Neotectonism and Crustal Stability, China Geological Survey, Beijing 100081, China

Funds: This research is financially supported by the Geological Survey Projects of the China Geological Survey (Grants DD20190306 and DD20190317).

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Received: 2022-05-29
Revised: 2022-10-09

Available Online: 2022-08-31

Abstract

Abstract

The Qionghua–Liantang fault belt, located at the boundary between the Fushan depression and the Haikou uplift, is the result of the impact of the uneven extension of the NE-trending Beibu Gulf rift. The Qionghua–Liantang fault belt passes through the Changliu New District and the major projects of the island-looping high-speed railway in Haikou, directly impacting the planning and construction of the Hainan Free Trade Zone. The article uses tectonic geomorphic survey, geophysical exploration, and drilling exploration to reveal that the Qionghua–Liantang fault consists of three NW-trending buried and semi-buried normal faults, which are the Wuyuanhe–Daoxincun fault (F1-1), the Yongzhuangshuiku fault (F1-2), and the Haikouzhuanwachang fault (F1-3). The width of the Qionghua–Liantang fault belt is about 1.8 km, and the length is about 17 km. The vertical displacement of the fault belt is 8.7~41.6 m since the Quaternary. The latest active age of these three faults is the late Pleistocene; the vertical activity rate was less than 0.1 mm/a. It is worth noting that the vertical activity rate of the Haikouzhuanwachang fault (F1-3) is higher than the other two faults and has more vigorous activity. Combining the tectonic background, the latest active age of the Qionghua–Liantang fault, and its relationship with Quaternary volcanic activity, this paper puts forward suggestions on the planning and construction of the Hainan Free Trade Zone and building avoidance of active fault.
- Qionghua–Liantang fault belt,
- fault activity,
- avoidance of active fault,
- Hainan,
- Quaternary period

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