Abstract
Landslides are important agents of the surface processes involved in the growth of mountainous topography. Dating prehistoric landslides is a prerequisite for establishing the relationships between prehistoric slope instability, and past climatic regimes and paleoseismic records. The Nyixoi Chongco rock avalanche (NCRA) is located in the Angang graben within the N–S trending rift zone in southern Tibet. It represents a giant prehistoric mass wasting event that was characterized by exceptional mobility and a large volume. However, the exact emplacement time and origin of the NCRA are still controversial. In this study, we conducted 14C dating of peat layers and snail shells to constrain the emplacement age of the NCRA. The 14C ages of the organic material and plant remnants in the basal peat layer are 1272–1389 and 1299–1404 cal AD, respectively. The 14C ages of aquatic snail shells and the bog overlying the rock avalanche are 425–565 and 1022–159 cal AD, respectively. These results indicate that the NCRA consisted of at least two separate and distinct events, instead of the single event suggested by previous studies. Based on field investigations and temporal correlations, we infer that there may be no paleoseismic records in the Angang graben that would corroborate a coseismic trigger for the NCRA. Therefore, we suggest that the 14C ages of the sediments below and above the landslide rocks should be interpreted carefully. The 14C ages alone do not provide sufficient evidence to infer the true trigger of the NCRA event.
Highlights
Rock avalanches are the result of the detachment of large volumes (>1 Mm3) of intact rock during extremely rapid, massive flow-like movements (Hungr et al, 2001)
A correlation between the Nyixoi Chongco rock avalanche (NCRA) and the Chubusi earthquake (1264 AD), which occurred outside the Angang graben, was proposed (Zeng et al, 2020)
A pit was dug from the surface down to the rock avalanche material, and snails and plant remnants were sampled for radiocarbon dating (Figure 5)
Summary
Rock avalanches are the result of the detachment of large volumes (>1 Mm3) of intact rock during extremely rapid, massive flow-like movements (Hungr et al, 2001). Reconstructing the occurrence history of rock avalanches is a key issue in discerning whether an increased incidence of such events can be expected in the future. To answer this question, it is important to identify the timing of past rock avalanche events and to correlate them with reconstructed seismic and/or climatic records. A correlation between the NCRA and the Chubusi earthquake (1264 AD), which occurred outside the Angang graben, was proposed (Zeng et al, 2020)
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