新疆阿克陶木吉盆地地质遗迹景观体系及成因研究  

Study on Landscape System and Genesis of Geological Relics in Muji Basin,Aktao County,Xinjiang

作　　者：张强 杨成 呼冬强 廖风云 范文龙 Zhang Qiang;Yang Cheng;Hu Dongqiang;Liao Fengyun;FanWenlong(Kashgar Geological Brigade of Xinjiang Uyghur Autonomous Region Geological Bureau,Kashgar,Xinjiang,844000,China;School of Mining Engineering and Geology,Xinjiang Institute of Engineering,Urumqi,Xinjiang,830023,China)

机构地区：[1]新疆维吾尔自治区地质局喀什地质大队,新疆喀什844000 [2]新疆工程学院矿业工程与地质学院,新疆乌鲁木齐830023

出　　处：《新疆地质》2024年第4期606-612,共7页Xinjiang Geology

基　　金：新疆维吾尔自治区地质局自筹资金项目新疆阿克陶县木吉乡地质遗迹保护利用研究(XGMB202350)项目资助。

摘　　要：新疆阿克陶县木吉乡地质遗迹资源丰富,通过对研究区内的250处地质遗迹进行研究分类,分析其地质特征及成因演化,总结分布规律。木吉地质遗迹中地貌景观大类在各地质大类中占比最大,数量最多,主要为岩土体地貌和水体地貌。木吉盆地地质遗迹分布特点是集中成群,泉华主要呈NW向串珠状分布于木吉河两岸Ⅰ级阶地;泥火山分布于木吉乡政府以北至帕斯布拉克村一带;碎屑岩地貌以风蚀雅丹为主,分布于木吉乡政府以北地区。泉华和泥火山的区别主要在于形成过程、喷发物质、喷发形态和地理分布等方面。Muji Township,Aketao County,Xinjiang is rich in geological relics resources.Through the study and classification of 250 geological relics in the study area,the geological characteristics and genetic evolution are analyzed,and the distribution law is summarized.The geomorphic landscape category in the geological relics of Muji accounts for the largest proportion and the largest number of geological categories,mainly rock and soil landforms and water landforms.The distribution characteristics of geological relics in Muji Basin are concentrated in groups,and the sinters are mainly distributed in the first-class terraces on both sides of Muji River in NW direction.The mud volcano is distributed from the north of Muji township government to Pasbrak village.The clastic rock landform is dominated by wind erosion Yardang,which is distributed in the north of Muji township government.The difference between spring and mud volcano is mainly in the formation process,eruption material,eruption form and geographical distribution.

关 键 词：地质遗迹 泉华 泥火山 地质成因 

分 类 号：P542.35[天文地球—构造地质学]