Meiyun 002 is an Ordinary Chondrite classified as L6, recovered in Guizhou, China in 2024. L‑group chondrites contain a lower metal content than H‑types and show a high degree of thermal metamorphism, where the original chondrules have been largely recrystallised into a more uniform, fine‑grained matrix. This texture reflects a parent body that experienced prolonged heating deep within an asteroid, causing early solar‑system material to blend, anneal, and stabilise while still preserving its fundamental chondritic chemistry. L6 specimens like Meiyun 002 are valued for illustrating the later stages of asteroidal evolution, where primitive rock transitions toward a more integrated, coherent structure. Energetically, L‑type chondrites are associated with grounding, stabilisation, and integrating long‑held patterns, supporting steady progress and inner organisation. Each specimen is housed in a clear acrylic display box (3.5 cm × 5.5 cm) with an identification label.
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1X MEIYUN 002 ORDINARY CHONDRITE METEORITE | APPROX 3CM
Meiyun 002 Ordinary Chondrite Meteorite - Guizhou, China 2024
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MEIYUN 002 ORDINARY CHONDRITE METEORITE
Meiyun 002 belongs to the L‑group of Ordinary Chondrites, a family of stony meteorites defined by their lower native‑metal content and balanced silicate chemistry. Classified as type L6, this specimen represents material that formed during the earliest stages of the solar system, originating from an asteroid whose interior developed under long‑term geological activity. L‑group meteorites are composed primarily of olivine and pyroxene, with accessory metal and sulfides distributed through the stone. Their chemistry provides important clues about the building blocks that shaped rocky planets and the conditions present in the protoplanetary disk. In energetic work, L‑type chondrites are often chosen for their steadying influence and their association with anchoring attention, organising thought, and supporting practical momentum.
