Liquefaction-Mudflow may Cause the Destruction of Prehistoric Lajia Ruins,China  

作　　者：Haijun Qiu Yingdong Wei Ulrich Kamp 

机构地区：[1]Shaanxi Key Laboratory of Earth Surface System and Environmental Carrying Capacity,College of Urban and Environmental Sciences,Northwest University,Xi’an,710127,China [2]Institute of Earth Surface System and Hazards,Northwest University,Xi’an,710127,China [3]Earth and Environmental Sciences Discipline,Department of Natural Sciences,University of Michigan-Dearborn,Dearborn,MI,48104,USA

出　　处：《Journal of Earth Science》2024年第6期2154-2157,共4页地球科学学刊（英文版）

基　　金：funded by the National Natural Science Foundation of China(No.42271078);the Key Research and Development Program of Shaanxi(No.2024SF-YBXM669)。

摘　　要：0 INTRODUCTION The Lajia Site in Guanting Basin in the Upper Reaches of the Yellow River,China,is known as the'Pompeii of the East'.It is adjacent to Xunhua and Hualong counties,and is also situated in the transitional zone between the Tibetan Plateau and the Loess Plateau(Figures 1a and 1b)(Wei et al.,2024).

关 键 词：situated transitional TIBETAN 

分 类 号：P642.23[天文地球—工程地质学] K878[天文地球—地质矿产勘探]