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Geoscience ›› 2025, Vol. 39 ›› Issue (01): 183-193.DOI: 10.19657/j.geoscience.1000-8527.2025.006

• Gemstone Geology • Previous Articles     Next Articles

Gem and Mineralogy, Chronology and Genesis of “Panlong Dark Jade” from Jilin Province

AN Wenjing1(), BAI Feng1(), LIU Mengsong1, ZHANG Daoyuan1, HUANG Tiantian1, WANG Wen2   

  1. 1. School of Gemology, China University of Geosciences (Beijing), Beijing 100083, China
    2. Jilin Sanhe Mining Exploiting Co., Ltd, Changchun, Jilin 130000, China
  • Online:2025-02-10 Published:2025-02-20
  • Contact: BAI Feng

Abstract:

This study systematically explores the gemological properties, genesis, and geological context of “Panglong Dark Jade”, aiming to elucidate its formation mechanisms and address existing research deficiencies in this area. Utilizing a multifaceted approach, we employed conventional gemological testing alongside various spectroscopic methods such as X-ray diffraction (XRD), laser Raman spectroscopy, and infrared spectroscopy as well as whole-rock chemical analysis and laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) for zircon U-Pb dating. Our focus was on “Panglong Dark Jade” discovered in the surrounding rocks of a medium-sized lead-zinc ore deposit in the east-central region of Jilin Province. The findings reveal that “Panglong Dark Jade” has a refractive index ranging from 1.53 to 1.54, a relative density of 2.73 to 2.79, and a Mohs hardness between 3.89 and 6.23. The primary mineral constituents are quartz and sericite, potentially accompanied by accessory minerals such as chlorite, pyrrhotite, and ilmenite. Its structural characteristics are marked by distinct slaty and massive forms, in addition to supermylonitic, aphanitic, and palimpsest textures. The main chromogenic minerals are predominantly graphite and chlorite. The total concentration of rare earth elements fluctuates between 177.93×10-6 and 216.89×10-6 revealing a significant enrichment of light rare earth elements alongside a pronounced deficit of Europium (Eu). Zircon U-Pb dating yields an age of (331.3±2.3) Ma, corresponding to the Middle Carboniferous Epoch. Integrating regional structural analyses with geological data suggests that the parent rock of “Panglong Dark Jade” is a normal sedimentary rock that underwent regional metamorphism to form carbonaceous slate, subsequently modified by hydrothermal activity to produce “Panglong Dark Jade”.

Key words: “Panlong Dark Jade”, gemological mineralogy, geochemistry, zircon U-Pb dating, chlorite-mica-quartz jade

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