Earth Science Frontiers ›› 2025, Vol. 32 ›› Issue (1): 127-141.DOI: 10.13745/j.esf.sf.2024.10.32

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Geochemical distribution of Li/Be in Pakistan: Implications for Li/Be prospecting

HONG Jun1,2(), Tahseenullah KHAN3, LI Wenyuan1,2, Yasir Shaheen KHALIL4, MA Zhongping1,2, ZHANG Jing2, WANG Zhihua2, ZHANG Huishan2, ZHANG Haidi2, LIU Chang2, Asad Ali NAREJO4   

  1. 1. MNR Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, Xi’an 710054, China
    2. Xi’an Center of Geological Survey, China Geological Survey, Xi’an 710054, China
    3. School of Earth and Environmental Sciences, Bahria University, Islamabad 44000, Pakistan
    4. Geological Survey of Pakistan, Islamabad 44000, Pakistan
  • Received:2024-08-01 Revised:2024-10-10 Online:2025-01-25 Published:2025-01-15

Abstract:

Lithium (Li) and beryllium (Be) are strategic metal resources with significant applications in emerging industries such as new materials and information technology. Pakistan is located at the convergence of the Eurasian, Indian and Arabian tectonic plates with favorable Li/Be mineralization conditions. However, due to limited geological investigations the full scope of Li/Be resource potential in Pakistan remains unknown. Low-density geochemical survey (1∶1 million scale) is an effective method for the study of Li/Be mineral distribution and rapid delineation of Li/Be prospective areas. In this paper, the geochemical background of Li/Be in Pakistan is analyzed based on a 1∶1 million low-density geochemical survey. Combined with analysis of the geological background of Li/Be mineralization, the paper aims to determine the prospective areas of Li/Be ore deposits to provide a basis for the prospecting and exploration of rare metal resources in Pakistan. In stream sediments of outcrop areas throughout Pakistan, Li concentrations ranged from 1.56 to 118.2 μg/g, with an average of 20.06 μg/g, while Be concentrations ranged from 0.07 to 7.16 μg/g, averaging 1.22 μg/g. Using 92% cumulative frequency data, 18 lithium and 12 beryllium geochemical anomaly areas were delineated, and prospective areas were selected accordingly. The Karakorum terrane and the Himalayan Fold Belt were identified as prospective areas for pegmatite-type lithium ore deposits, while the eastern part of the Chagai magmatic arc was identified for saline brine-type lithium ore deposits. The Karakorum terrane was found to be the most favorable area for further exploration of lithium and beryllium mineral resources.

Key words: lithium and beryllium, rare metals, resource potential, geochemical survey, prospective areas prediction, Pakistan

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