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作 者:Xiao-jian Zhao Nuo Li Kai Weng Ming Wang Qing-lin Sui Deng-hui Chen Zhou-ping Guo Meng-qi Jin
机构地区:[1]Xi’an Center,China Geological Survey,Ministry of Natural Resources,Xi’an 710054,China [2]Xinjiang Research Center for Mineral Resources,Xinjiang Institute of Ecology and Geography,Chinese Academy of Sciences,Urumqi 830011,China [3]College of Geography and Remote Sensing Sciences,Xinjiang University,Urumqi 830046,China [4]University of Chinese Academy of Sciences,Beijing 100029,China [5]No.8 Geological Party,Xinjiang Bureau of Geology and Mineral Exploration and Development,Aksu 843000,China [6]School of Resource&Environment and Safety Engineering,University of South China,Hengyang 421001,China
出 处:《China Geology》2024年第1期150-152,共3页中国地质(英文)
基 金:Supported by the Second Tibetan Plateau Scientific Expedition and Research(2021QZKK0303);the Natural Science Basic Research Program of Shaanxi(2020JQ-440 and 2021JQ-327);the Major Science and Technology Project of Xinjiang Uygur Autonomous Region(2021A03001-2);the projects of the China Geological Survey(DD20230333 and DD20230048).
摘 要:1.Objective In the past decade,a group of medium to giant lead-zinc deposits,represented by Huoshaoyun,Sachakou,and Yuanbaoling,have been discovered in the Aksai Chin region of Karakoram,Xinjiang.They are all located in the Mesozoic carbonate and clastic rock formations.The Sachakou leadzinc mining area is adjacent to the northwest of the Huoshaoyun lead-zinc mining area and is in the same stratigraphic layer as Huoshaoyun.Although many scholars have been arguing about the type and age of Huoshaoyun lead-zinc mineralization,few scholars have paid attention to the classification of the ore-bearing strata in the area.The stratigraphy of the Lower Permian Shenxianwan Group to the Upper Cretaceous Tielongtan Group is exposed in the Sachakou area of Karakorum,Xinjiang,however,the Late Permian-Early Triassic stratigraphy is missing(Fig.1a).Due to the harsh natural conditions in the area and the low level of work,the stratigraphic delineation is not exhaustive,and the regional lithology is dominated by carbonates and clastic rocks,which makes it difficult to identify the age of the regional lithology and causes problems for the exploration and research of lead-zinc in the area.
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