Distribution Pattern of Landslides Triggered by the 2014 Ludian Earthquake of China: Implications for Regional Threshold Topography and the Seismogenic Fault Identification

Suhua Zhou,Guangqi Chen,Ligang Fang

doi:10.3390/ijgi5040046

Suhua Zhou, Guangqi Chen + Show 1 more

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https://doi.org/10.3390/ijgi5040046

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Abstract

The 3 August 2014 Ludian earthquake with a moment magnitude scale (Mw) of 6.1 induced widespread landslides in the Ludian County and its vicinity. This paper presents a preliminary analysis of the distribution patterns and characteristics of these co-seismic landslides. In total, 1826 landslides with a total area of 19.12 km2 triggered by the 3 August 2014 Ludian earthquake were visually interpreted using high-resolution aerial photos and Landsat-8 images. The sizes of the landslides were, in general, much smaller than those triggered by the 2008 Wenchuan earthquake. The main types of landslides were rock falls and shallow, disrupted landslides from steep slopes. These landslides were unevenly distributed within the study area and concentrated within an elliptical area with a 25-km NW–SE striking long axis and a 15-km NW–SE striking short axis. Three indexes including landslides number (LN), landslide area ratio (LAR), and landslide density (LD) were employed to analyze the relation between the landslide distribution and several factors, including lithology, elevation, slope, aspect, distance to epicenter and distance to the active fault. The results show that slopes consisting of deeply weathered and fractured sandstones and mudstones were the more susceptible to co-seismic landslides. The elevation range of high landslide susceptibility was between 900–1300 m and 1800–2000 m. There was a generally positive correlation between co-seismic landslides and slope angle, until a maximum for the slope class 40°–50°. The co-seismic landslides occurred preferably on Southeast (SE), South (S) and Southwest (SW) oriented slopes. Results also show that the landslide concentration tends to decrease with distance from the surface projection of the epicenter rather than the seismogenic fault, and the highest landslide concentration is located within a 5–6 km distance of the seismogenic fault. Regarding the epicenter, the largest landslide clusters were found on the SE, northeast by east (NEE) and nearly West (W) of the epicenter. In addition, we also suggest that statistical results of slope gradients of landslides might imply a threshold topography of the study area within a tectonically active background. By analogy with other events, the statistical results of landslides aspects also imply the seismogenic fault of the Ludian earthquake might have been the Northwest (NW)-trending fault, which is consistent with other studies.

Highlights

According to the China Earthquake Network Center (CNEC) [1], an earthquake of Mw 6.1 hit the area between the Ludian County, the Qiaojia County and Huize County of Yunnan Province, at 4:30 p.m. (Beijing Time UTC+8) on 3 August 2014
According to China Earthquake Administration (CEA), in total, this earthquake affected 1,088,800 people and as of time 10:30 a.m. on 6 August, the earthquake had caused 589 deaths, 2,401 injuries, 80,900 buildings belonging to 25,800 families to collapse and serious damage to 129,100 buildings belonging to 40,600 families [2]
1826 landslides with a total area of 19.12 km2 triggered by the Ludian earthquake were mapped through visual interpretation of high-resolution aerial photos and Landsat-8 satellite images

Summary

Introduction

According to the China Earthquake Network Center (CNEC) [1], an earthquake of Mw 6.1 hit the area between the Ludian County, the Qiaojia County and Huize County of Yunnan Province, at 4:30 p.m. (Beijing Time UTC+8) on 3 August 2014. (Beijing Time UTC+8) on 3 August 2014. According to the China Earthquake Network Center (CNEC) [1], an earthquake of Mw 6.1 hit the area between the Ludian County, the Qiaojia County and Huize County of Yunnan Province, at 4:30 p.m. The epicenter of this earthquake was located at 27.11 ̋N, 103.13 ̋E, with a shallow focal depth of 12 km and a maximum intensity of IV in the area around the epicenter. According to China Earthquake Administration (CEA), in total, this earthquake affected 1,088,800 people and as of time 10:30 a.m. on 6 August, the earthquake had caused 589 deaths, 2,401 injuries, 80,900 buildings belonging to 25,800 families to collapse and serious damage to 129,100 buildings belonging to 40,600 families [2].

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